新疆东准噶尔纸房地区早古生代花岗岩的确定及其地质意义

徐芹芹; 赵磊; 牛宝贵

新疆东准噶尔纸房地区早古生代花岗岩的确定及其地质意义

中国地质科学院地质研究所, 北京 100037

基金项目:

国家自然科学基金项目 41572206

中国地质调查局地质调查项目 12120115070301

详细信息

作者简介:
徐芹芹(1984-), 女, 助理研究员, 主要从事大陆变形与构造地貌研究。E-mail:qinqin2002dz1@163.com

通讯作者:
赵磊(1979-), 男, 副研究员, 主要从事区域大地构造研究。E-mail:jleiz@163.com

中图分类号: P597
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出版历程
- 收稿日期: 2015-06-14
- 刊出日期: 2015-04-01

DETERMINATION OF THE EARLY PALEOZOIC GRANITE IN ZHIFANG AREA, EAST JUNGGAR, XINJIANG AND ITS GEOLOGICAL IMPLICATIONS

Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

摘要

摘要: 纸房花岗岩体位于新疆东准噶尔卡拉麦里构造带北侧。该岩体侵入的最新地层为中-上奥陶统荒草坡群, 并被晚志留世及早泥盆世地层不整合覆盖。对纸房花岗岩进行锆石SHRIMP U-Pb定年, 获得的²⁰⁶Pb/²³⁸U加权平均年龄为(463±7)~(436±4) Ma, 表明该岩体形成于晚奥陶世-早志留世, 是早古生代岩浆活动的产物。对已有的区域地质资料、岩体侵位时代及其与围岩接触关系进行综合分析后认为, 纸房花岗岩体的形成时代大致对应于卡拉麦里构造带内区域性角度不整合的形成时间, 推测该岩体为早古生代造山过程中形成的花岗质岩石。高Sr、低Yb、弱的Eu负异常等地球化学特征也显示其为埃达克型同造山花岗岩。纸房地区早古生代同造山花岗岩的存在为东准噶尔卡拉麦里构造带早古生代造山作用的确认提供了证据。
- 花岗岩 /
- 锆石SHRIMP U-Pb定年 /
- 东准噶尔 /
- 早古生代 /
- 造山作用
Abstract: Zhifang granite pluton outcrops in the northern part of Kalamaili tectonic belt, East Junggar Xinjiang. The latest strata intruded by the granite pluton are the Middle-Upper Ordovician Huangcaopo formation and it is unconformably covered by the Upper Silurian and Lower Devonian strata. Zircon SHRIMP U-Pb data showed that the weighted mean ²⁰⁶Pb/²³⁸U age was (463±7)~(436±4) Ma, which indicated that the granite pluton was emplaced during Late Ordovician and Early Silurian and it was the product of the early Paleozoic magmatic activity. Combining the existing regional geological data, the emplacement age of the granite pluton and the contact relation with the country rocks, it is speculated that the forming time of the granite pluton roughly corresponds to that of the regional angular unconformity in the Kalamaili tectonic belt and the Zhifang granite pluton might be formed during the early Paleozoic orogenic stage. The geochemical characteristics of high Sr, low Yb and weak negative Eu anomalies also suggests that it is the Adak-type syn-orogenic granite. Therefore determination of the syn-orogenic granite in Zhifang defines the presence of early Paleozoic orogenesis in Kalamaili tectonic belt, East Junggar.
- granite /
- zircon SHRIMP U-Pb data /
- East Junggar /
- early Paleozoic /
- orogenesis

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图 1 新疆北部地区构造简图及东准噶尔酸性侵入岩分布图(据文献[17, 20]修改)

Figure 1. Tectonic sketch of northern Xinjiang and distribution of acidic intrusive rocks in East Junggar

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图 2 纸房北部地区地质图(据文献[41]修改)

Figure 2. Geological map of northern Zhifang area

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图 3 花岗岩野外照片

(a)花岗岩体侵位于中-上奥陶统荒草坡群(O_2-3hn)；(b)花岗岩体被下泥盆统卓木巴斯套组(D₁zh)不整合覆盖，形成花岗质砂砾岩；(c)采样点处下泥盆统卓木巴斯套组(D₁zh)与花岗岩体不整合接触；(d)花岗岩体之上的砾岩

Figure 3. Field photographs of the granite

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图 4 花岗岩体主量元素图解

(a) TAS图解^[42]；(b) Na₂O+K₂O-CaO vs. SiO₂图解^[43]；(c) FeO^T/(FeO^T+MgO) vs. SiO₂图解^[44]；(d) ASI vs. SiO₂图解^[44]；FeO^T=FeO+0.9Fe₂O₃, ASI=molecular Al/(Ca-1.67P+Na+K)

Figure 4. Selected major element diagrams of the granite

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图 5 纸房地区花岗岩稀土元素球粒陨石标准化配分型式图与微量元素原始地幔蛛网图(标准化数值据文献[45])

Figure 5. Chondrite-normalized rare earth element patterns and primitive mantle normalized trace element spider diagram of granites in Zhifang area, East Junggar

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图 6 花岗岩样品锆石阴极发光图像

Figure 6. Cathodoluminescence images of selected zircon from granites

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图 7 东准噶尔纸房地区花岗岩样品锆石SHRIMP U-Pb谐和图

Figure 7. Concordia plob of zircon SHRIMP U-Pb data of the granites in Zhifang area, East Junggar

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表 1 东准噶尔纸房地区花岗岩主量元素(%)分析结果

Table 1. Major element concentrations of granites in Zhifang area, East Junggar

样品号	SiO₂	TiO₂	Al₂O₃	Fe₂O₃^T	FeO	MgO	CaO	MnO	Na₂O	K₂O	P₂O₅	LOI	TOTAL
ZF-2	74.33	0.25	13.35	2.2	0.90	0.62	1.6	0.04	5.4	0.72	0.05	1.38	99.95
ZF-3	73.64	0.24	13.12	2.07	0.88	0.95	1.65	0.05	6.24	0.35	0.05	1.59	99.94
ZF-4	75.38	0.22	12.92	1.91	0.75	0.62	1.26	0.06	5.79	0.47	0.05	1.32	99.99
ZF-5	74.38	0.23	12.49	1.97	0.55	0.64	2.08	0.02	5.56	0.54	0.05	2.01	99.96
ZF-7	73.28	0.24	13.76	2.10	0.68	0.66	1.61	0.06	4.75	2.24	0.06	1.20	99.96

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表 2 东准噶尔纸房地区花岗岩微量元素(×10^-6)分析结果

Table 2. Trace element concentrations of granites in Zhifang area, East Junggar

样品号	Li	Be	Sc	V	Cr	Co	Ni	Cu	Zn	Ga	Rb	Sr	Y	Zr	Nb	Cs	Ba	La	Ce	Pr	Nd	Sm	Eu
ZF-2	5.09	0.72	4.46	20.2	4.39	2.75	0.60	1.36	12.1	11.4	6.8	494	13.4	98.7	3.36	0.09	538	15.7	34.1	3.46	12.3	2.39	0.68
ZF-3	7.50	0.75	4.52	31.6	1.36	3.12	2.46	7.97	19.1	11.0	3.0	506	15.4	102	3.31	0.08	153	16.9	40.5	3.95	14.1	2.87	0.67
ZF-4	5.30	0.63	4.14	20.6	0.86	2.52	0.65	1.21	17.7	10.9	4.3	778	13.7	91.9	3.03	0.08	110	16.1	37.2	3.63	13.0	2.57	0.75
ZF-5	4.65	0.77	4.38	23.3	0.96	2.58	0.65	1.01	9.7	10.1	4.5	790	12.7	86.7	3.04	0.13	113	13.9	32.3	3.18	11.4	2.31	0.63
ZF-7	4.54	0.91	4.93	22.3	0.79	2.82	0.57	1.42	20.4	12.6	17.3	340	15.3	105	3.54	0.11	1005	18.4	42.2	4.06	14.5	2.85	0.73

样品号	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu	Hf	Ta	Tl	Pb	Bi	Th	U	ΣREE	(La/Sm)_N		(Gd/Yb)_N		(La/Yb)_N		Eu/Eu^*
ZF-2	2.17	0.38	2.09	0.48	1.54	0.28	1.84	0.30	3.19	0.31	0.02	2.02	0.02	3.76	1.17	192.66	4.24		0.98		6.12		0.89
ZF-3	2.52	0.42	2.47	0.53	1.68	0.31	2.02	0.33	3.1	0.29	0.01	2.58	0.02	3.83	1.05	214.99	3.80		1.03		6.00		0.74
ZF-4	2.30	0.38	2.17	0.46	1.52	0.27	1.79	0.29	2.82	0.28	0.02	2.57	0.04	3.42	0.83	201.87	4.04		1.06		6.45		0.93
ZF-5	2.05	0.35	2.05	0.45	1.46	0.26	1.72	0.28	2.82	0.27	0.02	1.64	0.03	3.38	0.66	176.97	3.88		0.99		5.80		0.86
ZF-7	2.55	0.42	2.39	0.53	1.68	0.31	1.98	0.33	3.28	0.33	0.05	3.26	0.01	3.92	1.07	225.80	4.17		1.07		6.67		0.81

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表 3 东准噶尔纸房地区花岗岩锆石SHRIMP U-Pb年龄分析结果

Table 3. Zircon SHRIMP U-Pb data of the granites in Zhifang area, East Junggar

点号	²⁰⁶Pb_c/%	U/10^-6	Th/10^-6	Th/U	²⁰⁶Pb^*/10^-6	²⁰⁷Pb^/²⁰⁶Pb^	%	²⁰⁷Pb^*/²³⁵U	%	²⁰⁶Pb/²³⁸U	1σ	²⁰⁶Pb/²³⁸U年龄/Ma	1σ
ZF-2-1.1	0.46	152	85	0.58	9.5	0.05689	2.7	0.57	3.0	0.07253	1.4	451.4	6.0
ZF-2-2.1	0.87	105	42	0.41	6.6	0.05793	4.2	0.58	4.5	0.07222	1.5	449.5	6.5
ZF-2-3.1	0.41	122	56	0.47	7.7	0.05973	2.7	0.60	3.1	0.07323	1.5	455.6	6.6
ZF-2-4.1	2.54	97	43	0.46	6.3	0.05389	12.9	0.54	13.0	0.07328	1.6	455.9	7.2
ZF-2-5.1	0.70	94	40	0.44	5.9	0.05864	6.7	0.59	6.9	0.07270	1.6	452.4	6.9
ZF-2-6.1	0.80	136	85	0.65	8.6	0.05908	5.4	0.60	5.6	0.07329	1.4	456.0	6.3
ZF-2-7.1	1.32	150	83	0.57	9.8	0.05571	5.9	0.58	6.1	0.07496	1.5	465.9	6.6
ZF-2-8.1	1.19	91	41	0.46	6.0	0.05139	8.5	0.53	8.6	0.07523	1.7	467.6	7.5
ZF-2-9.1	0.62	105	50	0.49	6.7	0.05427	4.3	0.56	4.6	0.07420	1.5	461.4	6.6
ZF-2-10.1	1.40	104	46	0.46	6.7	0.05276	9.1	0.54	9.2	0.07405	1.6	460.5	6.9
ZF-2-11.1	0.69	134	78	0.61	8.6	0.05287	5.3	0.54	5.5	0.07463	1.4	464.0	6.3
ZF-2-12.1	0.00	155	97	0.65	9.9	0.05794	3.0	0.59	3.3	0.07436	1.5	462.4	6.7
ZF-3-1.1	0.69	108	53	0.51	6.9	0.05242	5.2	0.5	5.4	0.07401	1.5	460.3	6.6
ZF-3-2.1	0.80	110	62	0.58	7.1	0.05294	6.1	0.5	6.3	0.07444	1.5	462.8	6.7
ZF-3-3.1	0.82	97	43	0.46	6.4	0.05478	4.4	0.6	4.6	0.07617	1.6	473.2	7.3
ZF-3-4.1	0.18	269	180	0.69	17.2	0.05564	1.7	0.6	2.1	0.07412	1.3	461.0	5.7
ZF-3-5.1	1.55	168	102	0.63	10.9	0.05132	6.6	0.5	6.8	0.07424	1.6	461.7	7.1
ZF-3-6.1	1.03	162	134	0.85	10.3	0.05543	6.1	0.6	6.3	0.07316	1.4	455.2	6.2
ZF-3-7.1	0.80	207	174	0.87	13.7	0.05093	4.1	0.5	4.3	0.07667	1.4	476.2	6.2
ZF-3-8.1	0.92	137	74	0.56	9.1	0.05234	7.9	0.6	8.0	0.07624	1.5	473.6	6.8
ZF-3-9.1	1.60	141	76	0.56	8.9	0.04782	9.0	0.5	9.1	0.07201	1.5	448.3	6.5
ZF-7-1.1	0.35	127	67	0.54	7.6	0.05899	3.3	0.57	3.7	0.06973	1.9	434.5	7.8
ZF-7-3.1	0.48	102	54	0.55	6.2	0.05924	4.2	0.58	4.5	0.07049	1.6	439.1	6.6
ZF-7-4.1	0.95	92	39	0.44	5.6	0.05470	4.9	0.53	5.5	0.06995	2.4	435.9	10.2
ZF-7-5.1	1.08	101	50	0.51	6.4	0.05211	9.4	0.52	9.5	0.07263	1.6	452.0	7.2
ZF-7-6.1	0.00	113	49	0.45	6.7	0.06264	4.4	0.60	4.9	0.06896	2.1	429.9	8.9
ZF-7-7.1	1.02	140	66	0.49	8.6	0.05362	2.9	0.52	3.4	0.07055	1.8	439.4	7.5
ZF-7-8.1	0.84	125	61	0.50	7.6	0.05047	6.8	0.49	6.9	0.07041	1.5	438.6	6.4
ZF-7-9.1	0.00	165	107	0.67	9.7	0.05393	2.9	0.51	3.3	0.06859	1.5	427.7	6.2
ZF-7-10.1	0.44	101	45	0.46	6.0	0.05748	4.0	0.54	4.3	0.06847	1.6	426.9	6.4
ZF-7-11.1	0.12	287	171	0.62	17.5	0.05680	1.9	0.56	2.3	0.07091	1.3	441.7	5.5
ZF-7-12.1	0.63	98	50	0.53	5.9	0.05568	5.2	0.53	5.5	0.06942	1.6	432.7	6.9
注：Pb_c和Pb^*分别表示普通铅和放射性成因铅

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