Geological and chronological characteristics of the Baiyin'gaolao Formation in Gaoyaowula, Inner Mongolia
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摘要: 通过1：50000区域地质调查，运用"火山构造-岩性岩相-火山地层"三重填图方法，将内蒙古东乌旗高尧乌拉白音高老组划分为3个岩性段，一段为火山碎屑沉积岩，二段为中性火山岩，三段为酸性火山岩，构成一个完整的沉积-喷发旋回。早期至晚期岩浆具有由中性向酸性演化的特征。划分出爆发相、侵出相、溢流相、火山通道相、喷发-沉积相及潜火山相等火山岩相；圈出12个Ⅴ级火山机构。获得高尧乌拉白音高老组二段粗安岩和三段流纹岩的LA-ICP-MS锆石U-Pb年龄分别为128.2±0.9 Ma和125.5±0.5 Ma，表明其形成时代为早白垩世。
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关键词:
- 白音高老组 /
- 火山作用 /
- LA-ICP-MS锆石U-Pb定年 /
- 高尧乌拉 /
- 内蒙古
Abstract: Based on a regional geological survey at a scale of 1:50000, it reveals that the volcanic rocks from the Baiyin'gaolao Formation of Gaoyaowula in Inner Mongolia could be divided into three lithologic segments by the triple mapping method of "volcanic structure-lithology and lithofacies-volcanic formation". The first lithologic segment is composed of pyroclastic sedimentary rocks, the second intermediate volcanic rocks and the third acidic volcanic rocks. The three lithologic segments constitute a complete depositonal-eruptive cycle, and the early to late magma is characterized by a transition from neutral to acid. The Baiyin'gaolao Formation can be classified into eruptive facies, intrusive facies, overflow facies, volcanic vent facies, eruption-deposition facies and subvolcanic facies, etc. Twelve V-grade volcanic apparatuses are delineated. The Zircon U-Pb LA-ICP-MS dating of the trachyandesite from the second lithologic segment of the Baiyin'gaolao Formation of Gaoyaowula and the rhyolite from the third are 128.2±0.9 Ma and 125.5±0.5 Ma respectively, indicating that the formation age is early-Cretaceous.-
Key words:
- Baiyin'gaolao Formation /
- volcanism /
- LA-ICP-MS zircon U-Pb dating /
- Gaoyaowula /
- Inner Mongolia
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图 1 研究区地质图
a—研究区大地构造位置示意图(据Jahn et al., 2004修改)；b—内蒙古东乌旗高尧乌拉地质图(李英杰等，2017)
Figure 1. Geological map of the research area
图 2 高尧乌拉白音高老组火山岩剖面图
1—安山质火山角砾岩；2—安山质岩屑晶屑凝灰岩；3—安山质晶屑凝灰岩；4—安山质含角砾熔结凝灰岩；5—含角砾粗安岩；6—粗安岩；7—流纹质火山角砾岩；8—流纹质晶屑凝灰岩；9—流纹岩；10—球粒流纹岩；11—黑曜岩；12—凝灰质砂岩；13—凝灰质砾岩；14—安山岩
Figure 2. Profile of volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula
图 3 高尧乌拉白音高老组火山岩野外及显微镜下照片
Pl—斜长石；Sa—透长石；Bt—黑云母；Q—石英
a—气孔状粗安岩野外露头；b—斑状结构粗安岩显微镜下照片(正交偏光下)；c—发育流动构造的流纹岩野外照片；d—发育流动构造的斑状结构流纹岩显微镜下照片(单偏光下)；e—发育球粒结构的球粒流纹岩野外露头；f—发育球粒结构的球粒流纹岩显微镜下照片(单偏光下)；g—少斑结构黑曜岩野外露头；h—少斑结构黑曜岩显微镜下照片(正交偏光)Figure 3. Outcrop photographs(left) and micrographs(right)of the volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula
图 4 内蒙古东乌旗高尧乌拉白音高老组二段粗安岩和三段流纹岩锆石阴极发光代表图像
a—二段粗安岩；b—三段流纹岩
Figure 4. Representative cathodoluminescent (CL) images of zircons for the trachyandesites and rhyolites from the Baiyin'gaolao Formation, Gaoyaowula
图 5 锆石U-Pb年龄谐和图和直方图
a—粗安岩锆石U-Pb年龄谐和图；b—粗安岩锆石U-Pb年龄直方图；c—流纹岩锆石U-Pb年龄谐和图；d—流纹岩锆石U-Pb年龄直方图
Figure 5. Zircon U-Pb concordia diagrams and histograms
图 6 高尧乌拉白音高老组火山岩TAS分类图
Figure 6. TAS diagram of the volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula
图 7 高尧乌拉白音高老组火山岩SiO2-K2O分类图解
Figure 7. SiO2 vs K2O classification diagram of the volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula
图 8 高尧乌拉白音高老组火山岩A/CNK-A/NK图
Figure 8. A/CNK-A/NK diagram of the volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula
图 9 高尧乌拉白音高老组火山岩稀土元素及微量元素特征
a—二段粗安岩稀土元素球粒陨石标准化配分曲线图(球粒陨石数据自Boynton，1984); b—二段粗安岩微量元素原始地幔标准化配分曲线图(原始地幔数据自Sun and McDonough, 1989); c—三段流纹岩稀土元素球粒陨石标准化配分曲线图(球粒陨石数据自Boynton，1984); d—三段流纹岩微量元素原始地幔标准化配分曲线图(原始地幔数据自Sun and McDonough, 1989)
Figure 9. Distribution pattern of rare earth elements and trace elements of the volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula
图 10 高尧乌拉白音高老组流纹岩构造环境判别图解
VAG—火山弧花岗岩；WPG—板内花岗岩；syn-COLG—同碰撞花岗岩；post-COLG—后碰撞花岗岩；ORG—大洋脊花岗岩；VAG+Syn-COLG—火山弧+同碰撞花岗岩
a—花岗岩类Y-Nb判别图; b—(Y+Nb)-Rb判别图(据Pearce et al., 1984修改)Figure 10. Discrimination diagrams showing the tectonic environment of the rhyolites from the Baiyin'gaolao Formation, Gaoyaowula
表 1 内蒙古高尧乌拉白音高老组火山岩实测剖面地层层序及韵律划分
Table 1. Stratigraphic sequence and rhythm classification of the measured section of the volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula
岩石地层单位 层号 岩性 分层厚度/m 组段厚度/m 形成方式 韵律划分 组 段 白音高老组 三段 17 紫色流纹质火山角砾岩 26.3 157.7 火山通道相 ⑥ 16 灰紫色条带状球粒流纹岩 21.5 溢流相 15 黑色黑曜岩 20.8 溢流相 14 灰紫色条带状球粒流纹岩 18.6 溢流相 13 灰紫色流纹岩 17.2 溢流相 12 灰紫色流纹质晶屑凝灰岩 11.6 空落堆积相 11 灰紫色流纹岩 21.7 溢流相 ⑤ 10 紫红色流纹质晶屑凝灰岩 10.3 空落堆积相 9 凝灰质砾岩 9.7 喷发-沉积相 ④ 二段 8 灰紫色安山质火山角砾岩 23.6 207 火山通道相 ③ 7 浅灰色含角砾粗安岩 57.4 溢流相 6 浅灰色安山质含角砾熔结凝灰岩 14.3 碎屑流堆积相 5 浅灰色安山质岩屑晶屑凝灰岩 32.9 空落堆积相 4 灰紫色粗安岩 52.1 溢流相 ② 3 浅灰色安山质晶屑凝灰岩 26.7 空落堆积相 一段 2 灰绿色凝灰质砂岩 11.9 30.1 火山沉积相 ① 1 浅灰色凝灰质砾岩 18.2 玛尼吐组 0 安山岩 溢流相 
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表 2 高尧乌拉白音高老组二段粗安岩和三段流纹岩LA-ICP-MS锆石U-Pb同位素分析结果
Table 2. LA-ICP-MS zircon U-Pb isotopic analysis of the trachyandesites and rhyolites from the Baiyin'gaolao Formation, Gaoyaowula
点号 元素含量/×10-6 Th/U 206Pb/238U 207Pb/235U 207Pb/206Pb 208Pb/232Th 206Pb/238U 207Pb/235U Th U 比值 1σ 比值 1σ 比值 1σ 比值 1σ 年龄/Ma ±1σ 年龄/Ma ±1σ 粗安岩(TW9846) 1 117 438 0.27 0.0200 0.0002 0.1339 0.0056 0.0486 0.0019 0.0080 0.0004 127 1 128 5 2 168 677 0.25 0.0201 0.0002 0.1354 0.0049 0.0489 0.0018 0.0094 0.0003 128 1 129 5 3 143 522 0.27 0.0197 0.0002 0.1472 0.0051 0.0542 0.0018 0.0070 0.0002 126 1 139 5 4 78 337 0.23 0.0197 0.0002 0.1288 0.0072 0.0473 0.0026 0.0088 0.0003 126 1 123 7 5 91 446 0.21 0.0200 0.0002 0.1436 0.0052 0.0521 0.0019 0.0080 0.0003 128 1 136 5 6 204 769 0.27 0.0201 0.0002 0.1382 0.0040 0.0498 0.0014 0.0077 0.0002 128 1 131 4 7 130 529 0.25 0.0199 0.0002 0.1472 0.0056 0.0535 0.0019 0.0075 0.0003 127 1 139 5 8 155 545 0.29 0.0199 0.0002 0.1279 0.0053 0.0466 0.0019 0.0078 0.0003 127 1 122 5 9 144 576 0.25 0.0202 0.0002 0.1471 0.0052 0.0528 0.0018 0.0088 0.0003 129 1 139 5 10 119 495 0.24 0.0206 0.0002 0.1528 0.0072 0.0539 0.0024 0.0100 0.0004 131 1 144 7 11 270 864 0.31 0.0200 0.0002 0.1395 0.0035 0.0505 0.0012 0.0081 0.0002 128 1 133 3 12 142 613 0.23 0.0206 0.0002 0.1561 0.0053 0.0549 0.0018 0.0098 0.0003 132 1 147 5 13 147 520 0.28 0.0203 0.0002 0.1361 0.0053 0.0486 0.0018 0.0078 0.0002 130 1 130 5 14 93 386 0.24 0.0204 0.0002 0.1461 0.0070 0.0520 0.0024 0.0090 0.0004 130 1 138 7 15 218 699 0.31 0.0203 0.0002 0.1432 0.0078 0.0512 0.0024 0.0085 0.0004 129 1 136 7 16 139 487 0.29 0.0205 0.0002 0.1521 0.0056 0.0539 0.0019 0.0090 0.0003 131 1 144 5 17 261 808 0.32 0.0202 0.0002 0.1465 0.0039 0.0525 0.0013 0.0082 0.0003 129 1 139 4 18 122 416 0.29 0.0210 0.0002 0.1517 0.0070 0.0524 0.0024 0.0095 0.0003 134 2 143 7 19 135 418 0.32 0.0198 0.0002 0.1329 0.0067 0.0487 0.0024 0.0074 0.0002 126 1 127 6 20 146 578 0.25 0.0198 0.0002 0.1350 0.0053 0.0495 0.0019 0.0072 0.0002 126 1 129 5 21 163 452 0.36 0.0197 0.0002 0.1389 0.0061 0.0512 0.0022 0.0065 0.0002 125 1 132 6 流纹岩(TW9850) 1 281 646 0.43 0.0193 0.0002 0.1325 0.0045 0.0499 0.0016 0.0050 0.0001 123 1 126 4 2 99 343 0.29 0.0197 0.0002 0.1452 0.0098 0.0533 0.0034 0.0070 0.0003 126 1 138 9 3 162 422 0.38 0.0196 0.0002 0.1435 0.0054 0.0530 0.0019 0.0040 0.0002 125 1 136 5 4 141 422 0.33 0.0195 0.0002 0.1314 0.0071 0.0488 0.0026 0.0067 0.0003 125 1 125 7 5 182 508 0.36 0.0198 0.0002 0.1520 0.0055 0.0557 0.0020 0.0070 0.0003 126 1 144 5 6 203 646 0.31 0.0197 0.0002 0.1617 0.0051 0.0595 0.0018 0.0080 0.0003 126 1 152 5 7 140 564 0.25 0.0196 0.0002 0.1343 0.0054 0.0497 0.0019 0.0073 0.0003 125 1 128 5 8 137 500 0.27 0.0197 0.0002 0.1357 0.0052 0.0500 0.0019 0.0075 0.0003 126 1 129 5 9 100 461 0.22 0.0197 0.0002 0.1347 0.0061 0.0495 0.0022 0.0076 0.0004 126 1 128 6 10 193 750 0.26 0.0195 0.0002 0.1395 0.0038 0.0518 0.0014 0.0082 0.0003 125 1 133 4 11 112 450 0.25 0.0200 0.0002 0.1463 0.0065 0.0531 0.0024 0.0090 0.0004 128 1 139 6 12 219 776 0.28 0.0196 0.0002 0.1316 0.0041 0.0486 0.0015 0.0088 0.0004 125 1 126 4 13 193 679 0.28 0.0197 0.0002 0.1521 0.0042 0.0560 0.0015 0.0090 0.0004 126 1 144 4 14 142 585 0.24 0.0195 0.0002 0.1371 0.0044 0.0510 0.0016 0.0084 0.0003 125 1 130 4 15 242 854 0.28 0.0198 0.0002 0.1339 0.0035 0.0491 0.0012 0.0077 0.0002 126 1 128 3 16 192 598 0.32 0.0195 0.0002 0.1323 0.0047 0.0491 0.0017 0.0078 0.0002 125 1 126 5 17 208 675 0.31 0.0196 0.0002 0.1364 0.0040 0.0504 0.0015 0.0079 0.0003 125 1 130 4
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表 3 高尧乌拉白音高老组二段粗安岩和三段流纹岩主量元素(%)和微量元素(×10-6)分析结果
Table 3. Major (wt%) and trace (×10-6) element analysis results of the trachyandesites and rhyolites from the Baiyin'gaolao Formation, Gaoyaowula
主量及
微量元素XT109
粗安岩XT109-2
粗安岩XT4524
粗安岩XT4525-2
粗安岩XT4503-1
粗安岩P35XT32
流纹岩P34XT09
流纹岩P43XT03
流纹岩XT4404
流纹岩P21XT17
流纹岩SiO2 57.45 59.02 62.40 64.11 63.89 76.02 76.60 76.37 77.87 76.51 TiO2 1.63 1.54 0.80 0.55 0.48 0.06 0.06 0.05 0.06 0.06 Al2O3 24.32 22.86 17.31 15.80 16.61 12.59 12.71 12.40 11.55 12.43 Fe2O3 1.43 0.80 4.37 4.46 3.48 0.79 0.76 0.32 1.04 0.93 FeO 1.81 2.52 0.55 0.52 0.62 0.25 0.07 0.18 0.08 0.22 MnO 0.130 0.130 0.160 0.089 0.095 0.04 0.04 0.02 0.02 0.02 MgO 0.75 0.71 0.68 1.03 0.99 0.15 0.08 0.13 0.07 0.08 CaO 1.15 1.60 4.53 2.85 1.45 0.50 0.43 0.96 0.47 0.44 Na2O 2.57 3.21 3.97 3.97 3.41 3.57 3.63 3.85 3.56 3.60 K2O 5.35 4.51 3.50 4.47 5.41 4.75 4.81 4.61 4.46 4.60 P2O5 0.28 0.35 0.29 0.19 0.20 0.03 0.02 0.02 0.02 0.02 LOI 2.90 2.61 1.29 1.82 3.21 1.22 0.74 1.05 0.76 1.01 TOTAL 99.80 99.85 99.84 99.84 99.82 99.96 99.95 99.95 99.97 99.93 Na2O+K2O 7.92 7.72 7.47 8.44 8.82 8.32 8.44 8.46 8.02 8.20 Mg# 30.67 28.66 21.94 29.58 32.43 22.33 16.68 32.29 10.31 12.55 La 31.9 39.3 18.4 21.1 20.7 25.21 31.53 20.41 29.87 36.63 Ce 34.1 29.9 27.1 30.6 26.1 45.68 57.33 36.71 51.33 62.91 Pr 58.6 57.1 53.5 54.3 57.2 5.99 7.71 5.28 6.82 9.48 Nd 9.07 8.90 6.77 7.10 6.06 22.14 28.63 20.36 25.77 35.90 Sm 7.72 7.88 5.14 5.09 4.34 3.82 5.50 4.07 4.87 6.85 Eu 1.49 1.65 1.39 1.38 1.27 0.28 0.36 0.27 0.44 0.41 Gd 6.27 6.77 4.37 4.35 3.88 3.04 4.39 3.48 4.26 5.34 Tb 1.03 1.14 0.69 0.71 0.65 0.47 0.74 0.60 0.73 0.85 Dy 6.03 6.82 3.6 3.97 3.57 2.50 4.10 3.34 4.17 4.42 Ho 1.14 1.30 0.70 0.77 0.72 0.49 0.81 0.66 0.86 0.83 Er 3.22 3.73 2.01 2.36 2.23 1.57 2.48 1.99 2.65 2.49 Tm 0.48 0.59 0.35 0.46 0.44 0.31 0.49 0.38 0.50 0.46 Yb 2.90 3.71 2.03 2.91 2.70 2.02 3.07 2.40 3.19 2.87 Lu 0.43 0.58 0.5 0.71 0.67 0.44 0.62 0.50 0.63 0.60 Y 31.9 39.3 18.4 21.1 20.7 14.21 23.55 18.61 27.19 23.49 Sc 16.7 18.2 13.0 9.9 5.5 2.80 2.62 2.15 2.72 2.14 Ni 9.10 10.4 3.08 2.03 2.35 1.99 0.30 0.91 0.41 1.52 Rb 78.0 79.8 96.1 146.0 187.0 160.66 151.57 139.15 155.83 132.60 Cr 12.5 19.1 25.8 19.3 7.2 2.83 1.23 2.84 3.27 4.30 Co 17.60 21.80 10.40 7.86 4.66 0.61 0.08 0.42 0.32 0.47 V 212.0 206.0 112.0 62.3 46.3 5.27 2.34 4.90 6.17 4.94 Zr 294 295 151 179 182 86.36 77.91 78.18 67.82 83.68 Hf 8.69 8.64 3.91 4.42 4.21 3.87 3.65 3.40 2.74 3.59 Ta 0.71 0.69 0.67 0.51 0.41 0.87 0.67 1.00 1.24 1.05 Sr 178 213 590 394 331 18.89 9.48 21.82 24.85 15.70 Ba 682 494 624 885 721 280.84 242.34 135.80 273 205.24 Nb 11.60 11.00 8.44 7.96 6.14 10.94 10.32 10.46 11.17 9.90 Cs 11.30 17.50 4.84 5.11 7.81 5.02 4.61 4.89 6.44 5.51 Ga 29.9 29.7 22.0 19.6 17.1 16.51 15.55 14.76 16.29 14.95 Pb 4.2 5.7 14.4 18.2 14.7 22.67 20.60 23.23 25.47 20.50 Th 8.87 8.41 7.35 8.61 6.96 11.69 9.95 13.16 15.00 12.87 U 2.17 2.35 1.92 2.19 2.78 4.58 3.16 3.00 3.28 3.06 ∑REE 164.38 169.37 126.55 135.81 130.53 113.96 147.76 100.45 136.09 170.04 LREE/HREE 6.65 5.87 7.88 7.36 7.78 9.51 7.85 6.52 7.01 8.52 (La/Yb)N 7.89 7.60 6.50 5.20 5.50 8.95 7.37 6.10 6.72 9.15 δEu 0.63 0.67 0.87 0.87 0.93 0.24 0.22 0.21 0.29 0.20
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ANDERSEN T, 2002. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 192(1-2): 59-79. doi: 10.1016/S0009-2541(02)00195-X BELOUSOVA E, GRIFFIN W, O'REILLY S Y, et al. , 2002. Igneous zircon: trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy and Petrology, 143(5): 602-622. doi: 10.1007/s00410-002-0364-7 BOYNTON W V, 1984. Cosmochemistry of the rare earth elements: meteorite studies[J]. Developments in Geochemistry, 2: 63-114. http://www.sciencedirect.com/science/article/pii/B9780444421487500083 CHEN J Y, FAN H H, WANG S Y, et al. , 2019. Ore-controlling factors of the Baerzhe super-large deposit in Jarud Banner, Inner Mongolia[J]. Journal of Geomechanics, 25(1): 27-35. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTotal-DZLX201901012.htm CHEN Y F, WANG G H, DUAN B X, 2012. Zircon SHRIMP geochronology and geochemistry of Late Jurassic volcanic rocks in Huiyin Obo area of Dong Ujimqin Banner, Inner Mongolia[J]. Geology in China, 39(6): 1690-1699. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI201206016.htm CHENG T S, YANG W J, WANG D H, et al. , 2012. Geological significance and geochemical characteristics of rhyolites in Baiyingaolao Formation at Halegaitu of Xiwuqi, Inner-Mongolia[J]. Journal of Liaoning Technical University (Natural Science), 31(4): 489-493. (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-FXKY201204014.htm CLAESSON S, VETRIN V, BAYANOVA T, et al. , 2000. U-Pb zircon ages from a Devonian carbonatite dyke, Kola peninsula, Russia: a record of geological evolution from the Archaean to the Palaeozoic[J]. Lithos, 51(1-2): 95-108. doi: 10.1016/S0024-4937(99)00076-6 COCKS L R M, TORSVIK T H, 2013. The dynamic evolution of the Palaeozoic geography of eastern Asia[J]. Earth-Science Reviews, 117: 40-79. doi: 10.1016/j.earscirev.2012.12.001 EBY G N, 1992. Chemical subdivision of the a-type granitoids: petrogenetic and tectonic implications[J]. Geology, 20(7): 641-644. doi: 10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2 GE W C, LIN Q, SUN D Y, et al. , 2000. Geochemical research into origins of two types of Mesozoic rhyolites in Daxing'anling[J]. Earth Science-Journal of China University of Geosciences, 25(2): 172-178. (in Chinese with English abstract) http://www.researchgate.net/publication/313219007_Geochemical_research_into_origins_of_two_types_of_Mesozoic_rhyolites_in_Daxing'anling Geological Department of Regional Geological and Mineral, 1987. Method guide of regional geological survey in volcanic rock area[M]. Beijing: Geological Publishing House. (in Chinese) GOU J, 2010. The geochronology and petrogenesis of volcanic rocks in Baiyinggaolao Formation from the southern Manzhouli, Inner-Mongolia[D]. Changchun: Jilin University. (in Chinese with English abstract) GOU J, SUN D Y, ZHAO Z H, et al. , 2010. Zircon LA-ICPMS U-Pb dating and petrogenesis of rhyolites in Baiyingaolao Formation from the southern Manzhouli, Inner-Mongolia[J]. Acta Petrologica Sinica, 26(1): 333-344. (in Chinese with English abstract) http://www.oalib.com/paper/1472934 HAO B, YANG X D, ZHANG M Y, et al. , 2011. Geochemical characteristics of upper Jurassic intermediate-granitic volcanic rocks from northern Chifeng, Inner Mongolia[J]. Journal of Geomechanics, 17(3): 274-285. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLX201103008.htm JAHN B M, WINDLEY B, NATAL'IN B, et al. , 2004. Phanerozoic continental growth in Central Asia[J]. Journal of Asian Earth Sciences, 23(5): 599-603. doi: 10.1016/S1367-9120(03)00124-X LI C M, 2009. A review on the minerageny and situ microanalytical dating techniques of zircons[J]. Geological Survey and Research, 32(3): 161-174. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ200903004.htm LI K, ZHANG Z C, LI J F, et al. , 2012. Zircon SHRIMP U-Pb age and geochemical characteristics of the Mesozoic volcanic rocks in Xi Ujimqin Banner, Inner Mongolia[J]. Geological Bulletin of China, 31(5): 671-685. (in Chinese with English abstract) http://www.researchgate.net/publication/285631907_Zircon_SHRIMP_U-Pb_age_and_geochemical_characteristics_of_the_Mesozoic_volcanic_rocks_in_Xi_Ujimqin_Banner_Inner_Mongolia LI W G, 1996. Stratigraphy (Lithostratic) of Nei Mongol autonomous region[M]. Beijing: China University of Geosciences Press. LI X Y, GUO F, FAN W M, et al. , 2004. Early Cretaceous trachytes of Donglingtai Formation from the Xishan area in the northern North China block: constraints on melting of lower mafic crust[J]. Geotectonica et Metallogenia, 28(2): 155-164. (in Chinese with English abstract) LI Y J, WANG G H, SANTOSH M, et al. , 2018. Supra-subduction zone ophiolites from Inner Mongolia, North China: implications for the tectonic history of the southeastern Central Asian orogenic belt[J]. Gondwana Research, 59: 126-143. doi: 10.1016/j.gr.2018.02.018 LI Y J, WANG G H, SANTOSH M, et al. , 2020. Subduction initiation of the SE Paleo-Asian Ocean: Evidence from a well preserved intra-oceanic forearc ophiolite fragment in central Inner Mongolia, North China[J]. Earth and Planetary Science Letters, 535: 116087. doi: 10.1016/j.epsl.2020.116087 LI Y J, WANG J F, LI H Y, et al. , 2012. Recognition of Diyanmiao ophiolite in Xi U jimqin Banner, Inner Mongolia[J]. Acta Petrologica Sinica, 28(4): 1282-1290. LI Y J, WANG J F, LI H Y, et al., 2017. Regional geological survey report of 1: 50000 Gaoyaowula in Inner Mongolia[R]. Heibei GEO University. (in Chinese) LIN M, 2018. New progress in the study of stratigraphic sequence and epoch of Baiyin'gaolao Formation in Demohada basin, Inner Mongolia[J]. Geological Bulletin of China, 37(9): 1588-1598. (in Chinese with English abstract) http://www.researchgate.net/publication/329874519_New_progress_in_the_study_of_stratigraphic_sequence_and_epoch_of_Baiyin'gaolao_Formation_in_Demohada_basin_Inner_Mongolia LIU H T, ZHAI M G, LIU J M, et al. , 2002. The Mesozoic granitoids in the northern marginal region of North China Craton: evolution from post-collisional to anorogenic settings[J]. Acta Petrologica Sinica, 18(4): 433-448. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200204000.htm LIU H, YANG X D, HAO B, et al. , 2011. Geochemical characteristics and Tectonic setting of upper Jurassic Jurassic granite from northern Chifeng, Inner Mongolia[J]. Journal of Geomechanics, 17(3): 286-294. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLX201103009.htm LIU J H, LIU D Y, ZHANG Y H, et al. , 2011. Techniques for choosing target points during SHRIMP dating of zircon U-Pb ages[J]. Rock and Mineral Analysis, 30(3): 265-268. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-YKCS201103010.htm LIU Y S, HU Z C, GAO S, et al. , 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 257(1-2): 34-43. doi: 10.1016/j.chemgeo.2008.08.004 LU Q D, 2004. Research report on mapping method of "volcanic structure-Lithology and lithofacies-volcanic sequence"[M]. Fuzhou: Fujian Provincial Map Publishing House. (in Chinese) LUDWIG K R, 1991. ISOPLOT: a plotting and regression program for radiogenic-isotope data[R]. Commonwealth of Virginia: US Geological Survey Open-File Report, 91-445. LUDWIG K R, 2003. User's manual for Isoplot 3.00: a geochronological toolkit for Microsoft Excel[R]. Berkeley: Berkeley Geochronological Center, Special Publication, 4: 71. METELKIN D V, VERNIKOVSKY V A, KAZANSKY A Y, et al. , 2010. Late Mesozoic tectonics of Central Asia based on paleomagnetic evidence[J]. Gondwana Research, 18(2-3): 400-419. doi: 10.1016/j.gr.2009.12.008 MIAO L C, FAN W M, LIU D Y, et al. , 2008. Geochronology and geochemistry of the Hegenshan ophiolitic complex: implications for late-stage tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China[J]. Journal of Asian Earth Sciences, 2008, 32(5-6): 348-370. doi: 10.1016/j.jseaes.2007.11.005 MO X X, ZHAO Z D, DENG J F, et al. , 2003. Response of volcanism to the India-Asia collision[J]. Earth Science Frontiers, 10(3): 135-148. (in Chinese with English abstract) http://ci.nii.ac.jp/naid/10026542218 PEARCE J A, HARRIS N B W, TINDLE A G, 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 25(4): 956-983. doi: 10.1093/petrology/25.4.956 PEI Q M, ZHANG S T, Hayashi K I, et al. , 2018. Permo-Triassic granitoids of the Xing'an-Mongolia segment of the Central Asian orogenic belt, Northeast China: age, composition, and tectonic implications[J]. International Geology Review, 60(9): 1172-1194. doi: 10.1080/00206814.2017.1377121 SHAO J A, LIU F T, CHEN H, et al. , 2001. Relationship between Mesozoic Magmatism and Subduction in Da Hinggan-Yanshan aera[J]. Acta Geologica Sinica, 75(1): 56-63. (in Chinese with English abstract) http://www.cqvip.com/QK/86253X/20011/1001445410.html SHAO J A, ZHANG L Q, MU B L, 1999a. Magmatism in the Mesozoic extending orogenic process of Da Hinggan MTS[J]. Earth Science Frontiers, 6(4): 339-346. (in Chinese with English abstract) http://ci.nii.ac.jp/naid/10008463139 SHAO J A, ZHAO G L, WANG Z, et al. , 1999b. Tectonic setting of Mesozoic volcanism in Da Hinggan Mountains, northeastern China[J]. Geological Review, 45(S1): 422-430. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP1999S1059.htm SHE H Q, LI J W, XIANG A P, et al. , 2012. U-Pb ages of the zircons from primary rocks in middle-northern Daxinganling and its implications to geotectonic evolution[J]. Acta Petrologica Sinica, 28(2): 571-594. (in Chinese with English abstract) http://www.zhangqiaokeyan.com/academic-journal-cn_acta-petrologica-sinica_thesis/0201252020277.html SI Q L, CUI T R, WANG D A, et al. , 2016. Zircon U-Pb dating and petrogenesis of the Baiyingaolao Formation rhyolites in Chaihe Area, great Xing'an range[J]. Journal of Northeastern University (Natural Science), 37(3): 412-415. (in Chinese with English abstract) http://www.researchgate.net/publication/301586227_Zircon_U-Pb_dating_and_petrogenesis_of_the_Baiyingaolao_Formation_rhyolites_in_Chaihe_area_Great_Xing'an_range SU W B, ZHANG S H, WARREN D, et al. , 2008. SHRIMP U-Pb ages of K-bentonite beds in the Xiamaling Formation: Implications for revised subdivision of the Meso-to Neoproterozoic history of the North China Craton[J]. Gondwana Research, 14(3): 543-553. doi: 10.1016/j.gr.2008.04.007 SUN D Y, WU F Y, GAO S, et al. , 2005. Confirmation of two episodes of A-type granite emplacement during Late Triassic and Early Jurassic in the central Jilin Province, and their constraints on the structural pattern of Eastern Jilin-Heilongjiang Area, China[J]. Earth Science Frontiers, 12(2): 263-275. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY20050200Z.htm SUN D Y, WU F Y, ZHANG Y B, et al. , 2004. The final closing time of the west Lamulun River-Changchun-Yanji plate suture zone-evidence from the Dayushan granitic pluton, Jilin Province[J]. Journal of Jilin University (Earth Science Edition), 34(2): 174-181. (in Chinese with English abstract) http://www.researchgate.net/publication/284701794_The_final_closing_time_of_the_west_Lamulun_River-Changchun-Yanji_plate_suture_zone_Evidence_from_the_Dayushan_granitic_pluton_Jilin_Province SUN S S, MCDONOUGH W F, 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 42(1): 313-345. doi: 10.1144/GSL.SP.1989.042.01.19 TAN H Y, HE Z H, CHEN F, et al. , 2017. Zircon U-Pb ages and geochemical characteristics of volcanic rocks in Baiyingaolao Formation of Suolun area within central Da Hinggan Mountains and their tectonic implications[J]. Geological Bulletin of China, 36(5): 893-908. (in Chinese with English abstract) http://www.researchgate.net/publication/319008952_Zircon_U-Pb_ages_and_geochemical_characteristics_of_volcanic_rocks_in_Baiyingaolao_Formation_of_Suolun_area_within_central_Da_Hinggan_Mountains_and_their_tectonic_implications TENG C, ZHANG X F, ZHOU Y, et al. , 2019. LA-ICP-MS zircon U-Pb age and geological significance of the Early Cretaceous Monzogranite in Xiaowulangou, Xilinhot, Inner Mongolia[J]. Geoscience, 33(5): 1003-1014. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTotal-XDDZ201905008.htm WANG C Y, SUN D Y, TIAN L H, et al. , 2018. Latest zircon U-Pb age of the Baiyingaolao Formation volcanic rocks in the Keyihe area of North-Central Da Hinggan Mountains[J]. ACTA Geologica Sinica, 92(5): 2034-2035. doi: 10.1111/1755-6724.13697 WANG F, ZHOU X H, Zhang L C, et al. , 2006. Late Mesozoic volcanism in the Great Xing'an Range (NE China): timing and implications for the dynamic setting of NE Asia[J]. Earth and Planetary Science Letters, 251(1-2): 179-198. doi: 10.1016/j.epsl.2006.09.007 WANG J G, HE Z H, XU W L, 2013. Petrogenesis of riebeckite rhyolites in the southern Da Hinggan Mts. : geohronological and geochemical evidence[J]. Acta Petrologica Sinica, 29(3): 853-863. (in Chinese with English abstract) http://www.oalib.com/paper/1475455 WANG Y, JI G Y, SUN S P, et al. , 2009. Origin of the volcanic rocks in the Donglingtai Formation from Yanhecheng area, western hills of Beijing and its geological implications[J]. Geological Review, 55(2): 191-214. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200902007.htm WHALEN J B, CURRIE K L, CHAPPELL B W, 1987. A-type granites: geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology volume, 95(4): 407-419. doi: 10.1007/BF00402202 XIAO W J, SUN M, SANTOSH M, 2015a. Continental reconstruction and metallogeny of the Circum-Junggar areas and termination of the southern Central Asian orogenic belt[J]. Geoscience Frontiers, 6(2): 137-140. doi: 10.1016/j.gsf.2014.11.003 XIAO W J, WINDLEY B F, HAN C M, et al. , 2018. Late Paleozoic to Early Triassic multiple roll-back and oroclinal bending of the Mongolia collage in Central Asia[J]. Earth-Science Reviews, 186: 94-128. doi: 10.1016/j.earscirev.2017.09.020 XIAO W J, WINDLEY B F, HAO J, et al. , 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: termination of the central Asian orogenic belt[J]. Tectonics, 22(6): 1069. http://petrology.oxfordjournals.org/external-ref?access_num=10.1029/2002TC001484&link_type=DOI XIAO W J, WINDLEY B F, HUANG B C, et al. , 2009. End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia[J]. International Journal of Earth Sciences, 98(6): 1189-1217. doi: 10.1007/s00531-008-0407-z XIAO W J, WINDLEY B F, SUN S, et al. , 2015b. A tale of amalgamation of three Permo-Triassic collage systems in Central Asia: oroclines, sutures, and terminal accretion[J]. Annual Review of Earth and Planetary Sciences, 43: 477-507. doi: 10.1146/annurev-earth-060614-105254 XU W L, WANG F, PEI F P, et al. , 2013. Mesozoic tectonic regimes and regional ore-forming background in NE China: constraints from spatial and temporal variations of Mesozoic volcanic rock associations[J]. Acta Petrologica Sinica, 29(2): 339-353. (in Chinese with English abstract) http://www.researchgate.net/publication/303919904_Mesozoic_tectonic_regimes_and_regional_ore-forming_background_in_NE_China_constraints_from_spatial_and_temporal_variations_of_Mesozoic_volcanic_rock_associations YING J F, ZHOU X H, ZHANG L C, et al. , 2010. Geochronological and geochemical investigation of the late Mesozoic volcanic rocks from the Northern Great Xing'an Range and their tectonic implications[J]. International Journal of Earth Sciences, 99(2): 357-378. doi: 10.1007/s00531-008-0395-z YUAN H L, GAO S, LIU X M, et al. , 2004. Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry[J]. Geostandards and Geoanalytical Research, 28(3): 353-370. doi: 10.1111/j.1751-908X.2004.tb00755.x ZHANG B T, WU J Q, LING H F, et al. , 2011. Elemental geochemical evidence for genesis of intraplate shoshonite and mantle-derived fluid metasomatism: Shoshonite from Huichang, Southern Jiangxi Province as an example[J]. Geochimica, 40(5): 443-453. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX201105005.htm ZHANG J H, 2009. Chronology and geochemistry of the Mesozoic volcanic rocks in the Great Xing'an Range, northeastern China[D]. Wuhan: China University of Geosciences (Wuhan). (in Chinese with English abstract) ZHANG J H, GE W C, WU F Y, et al. , 2008a. Large-scale Early Cretaceous volcanic events in the northern Great Xing'an Range, northeastern China[J]. Lithos, 102(1-2): 138-157. doi: 10.1016/j.lithos.2007.08.011 ZHANG L C, ZHOU X H, YING J F, et al. , 2008b. Geochemistry and Sr-Nd-Pb-Hf isotopes of Early Cretaceous basalts from the Great Xinggan Range, NE China: implications for their origin and mantle source characteristics[J]. Chemical Geology, 256(1-2): 12-23. doi: 10.1016/j.chemgeo.2008.07.004 ZHANG L T, LI S C, ZHAO Q Y, et al. , 2015. Formation age and geochemical characteristics of volcanic rocks from Baiyingaolao Formation of middle Da Hinggan Mountains[J]. Global Geology, 34(1): 44-54. (in Chinese with English abstract) http://d.wanfangdata.com.cn/Periodical/sjdz201501007 ZHANG Q, 2013. The criteria and discrimination for A-type granites: a reply to the question put forward by Wang Yang and some other persons for "A-type granite: what is the essence?"[J]. Acta Petrologica et Mineralogica, 32(2): 267-274. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201302014.htm ZHANG Q, 2018. Is the Mesozoic magmatism in eastern China related to the westward subduction of the Pacific plate?[J]. Acta Petrologica et Mineralogica, 32(1): 113-128. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201301011.htm ZHANG Q, RAN H, LI C D, 2012. A-type granite: what is the essence?[J]. Acta Petrologica et Mineralogica, 31(4): 621-626. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201204015.htm ZHANG X X, GAO Y F, LEI S H, 2016. Zircon U-Pb age and geochemistry of shoshonitic rocks from the Manitu Formation in the Honggeer area, central Inner Mongolia and their geological significance[J]. Geochimica, 45(4): 356-373. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX201604002.htm ZHANG Y Q, DONG S W, 2019. East Asia multi-plate convergence in Late Mesozoic and the development of continental tectonic systems[J]. Journal of Geomechanics, 25(5): 613-641. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTotal-DZLX201905004.htm ZUZA A V, YIN A, 2017. Balkatach hypothesis: a new model for the evolution of the Pacific, Tethyan, and Paleo-Asian oceanic domains[J]. Geosphere, 13(5): 1664-1712. doi: 10.1130/GES01463.1 陈金勇, 范洪海, 王生云, 等, 2019. 内蒙古扎鲁特旗巴尔哲超大型矿床控矿因素分析[J]. 地质力学学报, 25(1): 27-35. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20190104&journal_id=dzlxxb 陈英富, 王根厚, 段炳鑫, 2012. 内蒙古东乌珠穆沁旗辉音敖包一带晚侏罗世火山岩特征及时代[J]. 中国地质, 39(6): 1690-1699. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201206016.htm 程天赦, 杨文静, 王登红, 等, 2012. 哈勒盖图地区白音高老组流纹岩岩石地球化学特征及其地质意义[J]. 辽宁工程技术大学学报(自然科学版), 31(4): 489-493. https://www.cnki.com.cn/Article/CJFDTOTAL-FXKY201204014.htm 葛文春, 林强, 孙德有, 等, 2000. 大兴安岭中生代两类流纹岩成因的地球化学研究[J]. 地球科学-中国地质大学学报, 25(2): 172-178. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200002012.htm 苟军, 2010. 满洲里南部白音高老组火山岩的形成时代与岩石成因[D]. 长春: 吉林大学. 苟军, 孙德有, 赵忠华, 等, 2010. 满洲里南部白音高老组流纹岩锆石U-Pb定年及岩石成因[J]. 岩石学报, 26(1): 333-344. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201001038.htm 郝彬, 杨欣德, 张明洋, 等, 2011. 内蒙古赤峰北部晚侏罗世中酸性火山岩地球化学特征[J]. 地质力学学报, 17(3): 274-285. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20110307&journal_id=dzlxxb 李长民, 2009. 锆石成因矿物学与锆石微区定年综述[J]. 地质调查与研究, 32(3): 161-174. https://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200903004.htm 李可, 张志诚, 李建锋, 等, 2012. 内蒙古西乌珠穆沁旗地区中生代中酸性火山岩SHRIMP锆石U-Pb年龄和地球化学特征[J]. 地质通报, 31(5): 671-685. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201205005.htm 李文国, 1996. 内蒙古自治区岩石地层[M]. 北京: 中国地质大学出版社. 李晓勇, 郭锋, 范蔚茗, 等, 2004. 北京西山东岭台组粗面质火山岩地球化学: 下地壳熔融成因[J]. 大地构造与成矿学, 28(2): 155-164. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200402006.htm 李英杰, 王金芳, 李红阳, 等, 2012. 内蒙古西乌珠穆沁旗迪彦庙蛇绿岩的识别[J]. 岩石学报, 28(4): 1282-1290. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201204025.htm 李英杰, 王金芳, 李红阳, 等, 2017. 内蒙古1: 50000高尧乌拉幅区域地质调查报告[R]. 河北地质大学. 林敏, 2018. 内蒙古德莫哈达盆地白音高老组地层层序及时代研究新进展[J]. 地质通报, 37(9): 1588-1598. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201809004.htm 刘昊, 杨欣德, 郝彬, 等, 2011. 内蒙古赤峰北部晚侏罗世花岗岩地球化学特征及构造背景[J]. 地质力学学报, 17(3): 286-294. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20110308&journal_id=dzlxxb 刘红涛, 翟明国, 刘建明, 等, 2002. 华北克拉通北缘中生代花岗岩: 从碰撞后到非造山[J]. 岩石学报, 18(4): 433-448. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200204000.htm 刘建辉, 刘敦一, 张玉海, 等, 2011. 使用SHRIMP测定锆石铀-铅年龄的选点技巧[J]. 岩矿测试, 30(3): 265-268. https://www.cnki.com.cn/Article/CJFDTOTAL-YKCS201103010.htm 卢清地, 2004. "火山构造-岩性岩相-火山地层"填图方法研究报告[M]. 福州: 福建省地图出版社. 莫宣学, 赵志丹, 邓晋福, 等, 2003. 印度-亚洲大陆主碰撞过程的火山作用响应[J]. 地学前缘, 10(3): 135-148. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200303019.htm 区域地质矿产地质司, 1987. 火山岩地区区域地质调查方法指南[M]. 北京: 地质出版社. 邵济安, 张履桥, 牟保磊, 1999a. 大兴安岭中生代伸展造山过程中的岩浆作用[J]. 地学前缘, 6 (4): 339-346. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY199904025.htm 邵济安, 赵国龙, 王忠, 等, 1999b. 大兴安岭中生代火山活动构造背景[J]. 地质论评, 45(S1): 422-430. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP1999S1059.htm 邵济安, 刘福田, 陈辉, 等, 2001. 大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系[J]. 地质学报, 75(1): 56-63. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200101010.htm 佘宏全, 李进文, 向安平, 等, 2012. 大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系[J]. 岩石学报, 28(2): 71-594. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201202019.htm 司秋亮, 崔天日, 王恩德, 等, 2016. 大兴安岭柴河白音高老组流纹岩锆石U-Pb定年及成因探讨[J]. 东北大学学报(自然科学版), 37(3): 412-415. https://www.cnki.com.cn/Article/CJFDTOTAL-DBDX201603023.htm 孙德有, 吴福元, 张艳斌, 等, 2004. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间: 来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版), 34(2): 174-181. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200402003.htm 孙德有, 吴福元, 高山, 等, 2005. 吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J]. 地学前缘, 12(2): 263-275. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY20050200Z.htm 谭皓元, 和钟铧, 陈飞, 等, 2017. 大兴安岭中段索伦地区白音高老组火山岩锆石U-Pb年龄、地球化学特征及构造意义[J]. 地质通报, 36(5): 893-908. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201705022.htm 滕超, 张晓飞, 周毅, 等, 2019. 内蒙古锡林浩特小乌兰沟早白垩世二长花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 现代地质, 33(5): 1003-1014. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201905008.htm 王建国, 和钟铧, 许文良, 2013. 大兴安岭南部钠闪石流纹岩的岩石成因: 年代学和地球化学证据[J]. 岩石学报, 29(3): 853-863. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201303010.htm 汪洋, 姬广义, 孙善平, 等, 2009. 北京西山沿河城东岭台组火山岩成因及其地质意义[J]. 地质论评, 55(2): 191-214. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200902007.htm 许文良, 王枫, 裴福萍, 等, 2013. 中国东北中生代构造体制与区域成矿背景: 来自中生代火山岩组合时空变化的制约[J]. 岩石学报, 29(2): 339-353. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201302002.htm 章邦桐, 吴俊奇, 凌洪飞, 等, 2011. 板内橄榄玄粗岩(shoshonite)地幔流体交代作用及成因的元素地球化学证据: 以赣南会昌橄榄玄粗岩为例[J]. 地球化学, 40(5): 443-453. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX201105005.htm 张吉衡, 2009. 大兴安岭中生代火山岩年代学及地球化学研究[D]. 武汉: 中国地质大学(武汉). 张乐彤, 李世超, 赵庆英, 等, 2015. 大兴安岭中段白音高老组火山岩的形成时代及地球化学特征[J]. 世界地质, 34(1): 44-54. https://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ201501007.htm 张旗, 冉皞, 李承东, 2012. A型花岗岩的实质是什么?[J]. 岩石矿物学杂志, 31(4): 621-626. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201204015.htm 张旗, 2013. A型花岗岩的标志和判别: 兼答汪洋等对"A型花岗岩的实质是什么"的质疑[J]. 岩石矿物学杂志, 32(2): 267-274. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201302014.htm 张旗, 2018. 中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?[J]. 岩石矿物学杂志, 32(1): 113-128. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201301011.htm 张祥信, 高永丰, 雷世和, 2016. 内蒙古中部红格尔地区玛尼吐组钾玄质火山岩锆石U-Pb年龄、地球化学及其地质意义[J]. 地球化学, 45(4): 356-373. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX201604002.htm 张岳桥, 董树文, 2019. 晚中生代东亚多板块汇聚与大陆构造体系的发展[J]. 地质力学学报, 25(5): 613-641. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20190503&journal_id=dzlxxb -
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