塔里木盆地腹地玛扎塔格地区新近纪砂岩组分和重矿物组合特征及物源分析

李钦; 刘健

塔里木盆地腹地玛扎塔格地区新近纪砂岩组分和重矿物组合特征及物源分析

李钦,
刘健^,

中国地质科学院地质力学研究所, 北京 100081

基金项目:

特殊地质地貌区填图试点项目 DD20160060

塔里木盆地气候变化湖相沉积记录调查项目 12120113006200

详细信息

作者简介:
李钦(1991-), 男, 硕士研究生, 研究方向为盆地分析。E-mail:qinjelly555@126.com

通讯作者:
刘健(1970-), 男, 教授级高工, 主要从事构造地质学、沉积学等方面研究工作。E-mail:jianliu686@163.com

中图分类号: P512.2
计量
- 文章访问数: 362
- HTML全文浏览量: 250
- PDF下载量: 34
- 被引次数: 0
出版历程
- 收稿日期: 2016-08-11
- 刊出日期: 2017-04-01

ANALYSIS OF DETRITAL COMPOSITION, HEAVY MINERAL COMBINATION CHARATERISTICS AND SAND PROVENANCE OF NEOGENE SANDSTONES, MAZHATAGE MOUNTAIN IN THE CENTRE OF TARIM BASIN

LI Qin,
LIU Jian^,

Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

摘要

摘要: 发育于塔里木盆地腹地——玛扎塔格地区的新近纪沉积地层出露良好，保存了其物源区造山带的隆升剥蚀信息。利用古水流、砂岩碎屑组构和重矿物组合特征等研究方法，结合研究区的区域构造演化，探讨玛扎塔格地区晚新生代以来古地貌格局及沉积物源区隆升剥蚀的沉积响应关系。结果表明该研究区的古地貌总体格局为西高东低，沉积物源在上新世早期之前主要来自于西昆仑造山带和帕米尔造山带，而到了上新世以来其沉积物源主要来自于帕米尔造山带，并且在上新世早期，物源区发生明显的构造隆升运动，更新世期间物源区出现快速隆升剥蚀构造事件。
- 玛扎塔格 /
- 新近纪 /
- 古地貌 /
- 帕米尔高原 /
- 隆升剥蚀 /
- 青藏高原 /
- 西昆仑山脉
Abstract: Developed in the hinterland of the tarim basin, Neogene sedimentary stratain the centre of Tarim basin are well-outcropped and hold the information about the uplift and denudation of provenance orogenic belt.Using the methods of paleocurrent, sandstone detrital component and heavy mineral assemblages characteristics, combing with regional tectonic evolution of the study area, the sedimentary response relationship between the paleogeomorphology pattern and the uplifting and denudation of the sediment source area is discussed in Mazhatage Mountain. Results show that the overall pattern of the ancient landform in the study area is high in the west and low in the east, the sediment source of the study area before the early Pliocene mainly comes from the West Kunlun orogenic belt and Pamirsorogenic belt, while since the beginning of Pliocene epoch the sediment source mainly comes from Pamirs orogenic belt, and in the early Pliocenethere was an obvious structural uplift movement in the source area, and a rapid rise and denudation tectonic event occurred during the pleistocene period
- Mazhatage Mountain /
- Neogene /
- ancient landform /
- Pamirs /
- uplift and denudation /
- Tibet Plateau /
- West Kunlun Mountains

HTML全文

图 1 玛扎塔格地区及其物源区地质图^[7~8]

Figure 1. A geological map of Mazhatage and its provenance

下载: 全尺寸图片幻灯片

图 2 玛扎塔格剖面地层分布特征

图a中遥感影像中黑线的位置表示为剖面所在位置(剖面起点坐标位置为N 80°19′14.17″，E 38°42′04.75″：终点坐标位置为N 80°18′15.14″，E 38°40′51.61″)；图b为测量地质剖面图

Figure 2. Distributing characteristics of strata profile in Mazhatage

下载: 全尺寸图片幻灯片

图 3 野外考察照片

a—喀什群地层中的牡蛎化石b—乌恰群地层中发育的板状斜层理c—乌恰群—阿图什组界线d—阿图什组地层中发育的砂砾岩e—西域组地层中发育的水平层理f—西域组顶部地层中的硅化木化石

Figure 3. Pictures of field investigation

下载: 全尺寸图片幻灯片

图 4 沉积地层、砂岩碎屑组分和重矿物组合特征(年龄数据来自文献[2]

Figure 4. Sedimentary strata、sandstone detrital component and heavy mineral combination characteristics

下载: 全尺寸图片幻灯片

表 1 玛扎塔格剖面重矿物组合特征

Table 1. Heavy mineral combination characteristics of Mazartagh section

碎屑重矿物组合	物源岩石类型
石榴石、绿帘石	高级变质岩
辉石、角闪石、金红石	基性火山岩
角闪石、辉石、锆石、绿帘石	中性火山岩
角闪石、磷灰石、锆石	酸性火山岩
锆石、金红石、石榴石	沉积岩

下载: 导出CSV

参考文献(35)

[1]	Zheng H B, McAulay Powell C, An Z S, et al. Pliocene uplift of the northern Tibetan Plateau[J]. Geology, 2000, 28(8): 715~718. doi: 10.1130/0091-7613(2000)28<715:PUOTNT>2.0.CO;2
[2]	郑洪波, 贾军涛, 王可.塔里木盆地南缘新生代沉积:对青藏高原北缘隆升和塔克拉玛干沙漠演化的指示[J].地学前缘, 2009, 16(6): 154~161. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200906023.htm ZHENG Hong-bo, JIA Jun-tao, WANG Ke.Cenozoic sedimentation in the southern Tarim Basin: Implications for the uplift of northern Tibet and evolution of the Taklimakan Desert[J]. Earth Science Frontiers, 2009, 16(6): 154~161. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200906023.htm
[3]	Zheng H B, Wei X C, Tada R, et al. Late Oligocene-early Miocene birth of the Taklimakan Desert[J]. Proceedings of the National Academy of Sciences of the United States of America, 2015, 112(25): 7662~7667. doi: 10.1073/pnas.1424487112
[4]	Sun J M, Zhu R X, Bowler J. Timing of the Tianshan Mountains uplift constrained by magnetostratigraphic analysis of molassedeposits[J]. Earth and Planetary Science Letters, 2004, 219(3/4): 239~253. http://www.sciencedirect.com/science/article/pii/S0012821X04000081
[5]	Sun J M, Xu Q H, HuangB C. Late Cenozoic magnetochronology and paleoenvironmental changes in the northern foreland basin of the Tian Shan Mountains[J]. Journal of Geophysical Research:Solid Earth, 2007, 112(B4): B04107. doi: 10.1029/2006JB004653/full#footer-citing
[6]	Sun J M, Li Y, Zhang Z Q, et al. Magnetostratigraphic data on Neogene growth folding in the foreland basin of the southern Tianshan Mountains[J]. Geology, 2009, 37(11): 1051~1054. doi: 10.1130/G30278A.1
[7]	Thompson J A, Burbank D W, Li T, et al. Late Miocene northward propagation of the northeast Pamir thrust system, Northwest China[J]. Tectonics, 2015, 34(3): 510~534. doi: 10.1002/2014TC003690
[8]	Cao K, WangG C, van der Beek P, et al. Cenozoic thermo-tectonic evolution of the northeastern Pamir revealed by zircon and apatite fission-track thermochronology[J]. Tectonophysics, 2013, 589: 17~32. doi: 10.1016/j.tecto.2012.12.038
[9]	司家亮, 李海兵, Barrier L, 等.青藏高原西北缘晚新生代的隆升特征——来自西昆仑山前盆地的沉积学证据[J].地质通报, 2007, 26(10): 1356~1367. doi: 10.3969/j.issn.1671-2552.2007.10.013 SI Jia-liang, LI Hai-bing, Barrier L, et al. Late Cenozoic uplift of thenorthwestern margin of the Qinghai-Tibet Plateau: Sedimentary evidence from piedmont basins of the West Kunlun Mountains[J]. Geological Bulletin of China, 2007, 26(10): 1356~1367. doi: 10.3969/j.issn.1671-2552.2007.10.013
[10]	陈杰, 卢演俦, 丁国瑜.塔里木西缘晚新生代造山过程的记录——磨拉石建造及生长地层和生长不整合[J].第四纪研究, 2001, 21(6): 528~539. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200106009.htm CHEN Jie, LU Yan-chou, DING Guo-yu.Records of Late Cenozoic Mountain building in western Tarimbasin: molasses, growth strata and growth unconformity[J]. Quaternary Sciences, 2001, 21(6): 528~539. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200106009.htm
[11]	Chen J, Burbank D W, Scharer K M, et al. Magnetochronology of the Upper Cenozoic strata in the Southwestern Chinese TianShan: rates of Pleistocene folding and thrusting[J]. Earth and Planetary Science Letters, 2002, 195(1/2): 113~130. http://www.sciencedirect.com/science/article/pii/S0012821X01005799
[12]	陈杰, 李涛, 李文巧, 等.帕米尔构造结及邻区的晚新生代构造与现今变形[J].地震地质, 2011, 33(2): 241~259. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201102006.htm CHEN Jie, LI Tao, LI Wen-qiao, et al. Late Cenozoic and present tectonic deformation in the Pamirsalient, northwestern China[J]. Seismology and Geology, 2011, 33(2):241~259. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201102006.htm
[13]	潘家伟, 李海兵, Van Der WoerdJ, 等.西昆仑山前冲断带晚新生代构造地貌特征[J].地质通报, 2007, 26(10): 1368~1379. doi: 10.3969/j.issn.1671-2552.2007.10.014 PAN Jia-wei, LI Hai-bin, Van Der Woerd J, et al. Late Cenozoic morphotectonic features of the thrust belt in the front of the West Kunlun Mountains[J]. Geological Bulletin of China, 2007, 26(10): 1368~1379. doi: 10.3969/j.issn.1671-2552.2007.10.014
[14]	裴军令, 李海兵, 孙知明, 等.塔里木盆地腹地玛扎塔格山隆升时限探讨及其环境意义[J].岩石学报, 2011, 27(1): 333~343. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201101025.htm PEI Jun-ling, LI Hai-bin, SUN Zhi-ming, et al. Constraints the uplift age of MazaTaghMountain in the Centre of Tarim basin and its climatic implications[J]. ActaPetrologicaSinica, 2011, 27(1): 333~343. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201101025.htm
[15]	Charreau J, ChenY, Gilder S, et al. Magnetostratigraphy and rock magnetism of the NeogeneKuitun He section (northwest China): implications for Late Cenozoic uplift of the Tianshanmountains[J]. Earth and Planetary Science Letters, 2005, 230(1/2): 177~192.
[16]	Charreau J, Gilder S, Chen Y, et al. Magnetostratigraphy of the Yaha section, Tarim Basin (China): 11 Ma acceleration in erosion and uplift of the Tian Shan mountains[J]. Geology, 2006, 34(3): 181~184. doi: 10.1130/G22106.1
[17]	Hubert-Ferrari A, Suppe J, Gonzalez-Mieres R, et al. Mechanisms of active folding of the landscape (southern Tian Shan, China)[J]. Journal of Geophysical Research: Solid Earth, 2007, 112(B3): B03S09. doi: 10.1029/2006JB004362/references
[18]	Heermance R V, Chen J, Burbank D W, et al. Chronology and tectonic controls of Late Tertiary deposition in the southwestern Tian Shan foreland, NW China[J]. Basin Research, 2007, 19(4): 599~632. doi: 10.1111/bre.2007.19.issue-4
[19]	Robinson A C, Ducea M, Lapen T J. Detrital zircon and isotopic constraints on the crustal architecture and tectonic evolution of the northeastern Pamir[J]. Tectonics, 2012, 31(2): TC2016. doi: 10.1029/2011TC003013/full
[20]	Cowgill E, An Y, Harrison T M, et al. Reconstruction of the AltynTagh fault based on U-Pb geochronology: Role of back thrusts, mantle sutures, and heterogeneous crustal strength in forming the Tibetan Plateau[J]. Journal of Geophysical Research: Solid Earth, 2003, 108(B7): 2346.
[21]	Jiang Y H, Liao S Y, Yang W Z, et al. An island arc origin of plagiogranites at Oytag, western Kunlun orogen, northwest China: SHRIMP zircon U-Pb chronology, elemental and Sr-Nd-Hf isotopic geochemistry and Paleozoic tectonic implications[J]. Lithos, 2008, 106(3/4): 323~335. http://www.sciencedirect.com/science/article/pii/S0024493708001680
[22]	Schwab M, Ratschbacher L, Siebel W, et al. Assembly of the Pamirs: Age and origin of magmatic belts from the southern Tien Shan to the southern Pamirs and their relation to Tibet[J]. Tectonics, 2004, 23(4): TC4002.
[23]	司家亮, 李海兵, 裴军令, 等.塔里木盆地玛扎塔格第四纪沉积环境演变及构造学意义[J].岩石学报, 2011, 27(1): 321~332. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201101024.htm SI Jia-liang, LI Hai-bing, PEI Jun-ling, et al. Sedimentary environment variation and its tectonic significanceof MazarTagh in the middle Tarim basin[J]. Acta Petrologica Sinica, 2011, 27 (1): 321~332. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201101024.htm
[24]	雍天寿, 单金榜, 王诗佾.玛扎塔克山区的几个地质问题——兼谈塔克拉玛干大沙漠形成的地质时代[J].新疆石油地质, 1983, (4): 1~9. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD198304000.htm YONG Tian-shou, SHAN Jin-bang, WANG Shi-yi.Several problems on the geological aspects of theMazhatageMountain[J]. Xinjiang Petroleum Geology, 1983, (4): 1~9. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD198304000.htm
[25]	储书武, 李双应.两种砂岩碎屑组分统计方法的比较[J].合肥工业大学学报(自然科学版), 2007, 30(6): 668~671. http://www.cnki.com.cn/Article/CJFDTOTAL-HEFE200706002.htm CHU Shu-wu, LI Shuang-ying.Comparison between two methods for statistical study of detrital composition of sandstones[J]. Journal of Hefei University of Technology, 2007, 30(6): 668~671. http://www.cnki.com.cn/Article/CJFDTOTAL-HEFE200706002.htm
[26]	Dickinson W R. Interpreting provenance relations from detrital modes of sandstones[A]. Zuffa G G. Provenance of Arenites[M]. Netherlands: Netherlands, 1985: 333~361.
[27]	Morton A C, Todd Jr S P, Haughton P D W. Developments in sedimentary provenance studies[M]. London:Oxford UniversityPress, 1991.
[28]	郑超, 李宝芳, 温显端.秦岭北麓晚二叠世平顶山段辫状河-辫状三角洲沉积体系及其构造涵义[J].现代地质, 2003, 17(4): 415~420. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200304009.htm ZHENG Chao, LI Bao-fang, WEN Xian-duan.Depositional characteristics of the late permian braided channel-braided delta deposits in northern foothills of the Qinling Mountains, China[J]. Geoscience, 2003, 17(4): 415~420. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200304009.htm
[29]	杨仁超, 李进步, 樊爱萍, 等.陆源沉积岩物源分析研究进展与发展趋势[J].沉积学报, 2013, 31(1): 99~107. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201301012.htm YANG Ren-chao, LI Jin-bu, FAN An-ping, et al. Research progress and development tendency of provenance analysis on terrigenous sedimentary rocks[J]. Acta Sedimentologica Sinica, 2013, 31(1): 99~107. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201301012.htm
[30]	胡宗全, 朱筱敏, 彭勇民.准噶尔盆地西北缘车排子地区侏罗系物源及古水流分析[J].古地理学报, 2001, 3(3): 49~54. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200103006.htm HU Zong-quan, ZHU Xiao-min, PENG Yong-min. Analysis of provenance and Palaeocurrent direction of Jurassic at Chepaizi region in Northwest edge of Junggarbasin[J]. Journal of Palaeogeography, 2001, 3(3): 49~54. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200103006.htm
[31]	杜叶龙, 李双应, 孔为伦, 等.安徽东南部二叠系龙潭组砂岩碎屑组分及物源分析[J].高校地质学报, 2010, 16(4): 509~516. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201004012.htm DU Ye-long, LI Shuang-ying, KONG Wei-lun, et al. Sandstone detrital composition and provenance analysis of the Permian Longtan Formation in southeastern Anhui Province[J]. Geological Journal of China Universities, 2010, 16(4): 509~516. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201004012.htm
[32]	赵红格, 刘池洋.物源分析方法及研究进展[J].沉积学报, 2003, 21(3): 409~415. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200303006.htm ZHAO Hong-ge, LIU Chi-yang.Approaches and prospects of provenance analysis[J]. Acta Sedimentologica Sinica, 2003, 21(3): 409~415. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200303006.htm
[33]	Heller P L, Paola C. The large-scale dynamics of grain-size variation in alluvial basins, 2: Application to syntectonicconglomerate[J]. Basin Research, 1992, 4(2): 91~102. doi: 10.1111/bre.1992.4.issue-2
[34]	Paola C, Heller P L, Angevine C L. The large-scale dynamics of grain-size variation in alluvial basins, 1: Theory[J]. Basin Research, 1992, 4(2): 73~90. doi: 10.1111/bre.1992.4.issue-2
[35]	Sun J M, Jiang M S. Eocene seawater retreat from the southwest Tarim Basin and implications for early Cenozoic tectonic evolution in the Pamir Plateau[J]. Tectonophysics, 2013, 588: 27~38. doi: 10.1016/j.tecto.2012.11.031