东亚大陆西缘侏罗纪变形——以班公湖-怒江带中段韧性变形为例

施炜; 董树文; 黄兴富; 陈虹; 崔建军

东亚大陆西缘侏罗纪变形——以班公湖-怒江带中段韧性变形为例

1.
中国地质科学院地质力学研究所, 北京 100081
2.
南京大学地球科学与工程学院, 江苏南京 210093

基金项目:

国家重点研发计划项目 2017YFC0601402

中国地质调查局项目 1212011120184

中国地质调查局项目 1212011221111

详细信息

作者简介:
施炜(1971-), 男, 研究员, 主要从事中、新生代构造研究.E-mail:shiweinmg@163.com

中图分类号: P542
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- 被引次数: 0
出版历程
- 收稿日期: 2017-03-06
- 刊出日期: 2017-08-01

JURASSIC DEFORMATION AT THE WESTERN MARGIN OF THE EAST ASIA CONTINENT: A CASE STUDY OF DUCTILE DEFORMATION IN THE CENTRAL SEGMENT OF THE BANGONG CO-NUJIANG BELT

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, Jiangsu, China

摘要

摘要: 班公湖-怒江带作为羌塘地块与拉萨地块晚中生代聚合而形成巨型构造带，其形成时代与如何汇聚是构造研究关键所在。本次研究选择班公湖—怒江带中段的安多—聂荣地块发育为研究区，对地块内部基底发育的近东西走向的韧性剪切带，开展了韧性剪切变形分析与同构造年代学研究。剪切带面理和线理测量分析指示北东—南西向构造挤压，其同构造矿物⁴⁰Ar/³⁹Ar的测试分析获得年龄约为167 Ma，表明班公湖-怒江带中段形成于中侏罗世中期北东—南西向汇聚的构造背景下。结合区域构造分析，东亚大陆西缘羌塘地块与拉萨地块在中侏罗世中期以北东—南西向碰撞聚合的构造方式完成大陆拼接，为东亚大陆西缘中侏罗世变形提供了直接构造证据。
- 东亚大陆 /
- 班公湖—怒江带 /
- 安多—聂荣地块 /
- 韧性剪切变形 /
- 侏罗纪
Abstract: The Bangong Co-Nujiang belt resulted from the convergence and collision between the Chiangtang and Lhasa blocks in late Mesozoic. The key issue in this tectonic study is when and how the belt was formed. With the Ando-Nyainrong block of the central segment of the Bangong Co-Nujiang belt as the study area, the ductile shear belts with approximately E-W strike developed in the internal basement of the block are studied based on ductile shear deformation analysis and syntectonic geochronology. The foliation and lineation measurement and analysis of the shear belts indicate tectonic compression with NE-SW strike. Through the test analysis of ⁴⁰Ar/³⁹Ar in syntectonic minerals, the age is worked out as 167 Ma. All the evidence shows that the central segment of the Bangong Co-Nujiang belt was caused under the convergence and collision between the Chiangtang and Lhasa blocks in the middle of Middle Jurassic, which provides direct tectonic evidence for the Jurassic deformation at the western margin of the East Asian continent.
- East Asia continent /
- Bangong Co-Nujiang belt /
- Ando-Nyainrong block /
- ductile shear deformation /
- Jurassic

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图 1 青藏高原及其邻区构造纲要图与东亚大陆晚中生代构造简图

F₁—喜马拉雅主冲断层；F₂—雅鲁藏布江缝合带；F₃—班公湖-怒江缝合带；F₄—金沙江缝合带；F₅—昆仑山断裂带；F₆—阿尔金断裂带；F₇—海原-祁连山构造带；F₈—喀喇昆仑断裂带；F₉—龙门山断裂带

Figure 1. Tectonic outline map of the Qinghai-Tibet Plateau and its adjacent areas and simplified tectonic map of the East Asia continent in late Mesozoic

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图 2 班公湖—怒江缝合带中段地质简图^[70~71]

Figure 2. Geological sketch of the middle segment of the Bangong Co-Nujiang suture belt^[70~71]

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图 3 安多—聂荣地块韧性剪切带北东—南西向构造应力场特征(下半球等角投影(吴氏网))

Figure 3. The characteristics of the NE-SW direction tectonic stress field of the ductile shear belts in the Ando-Nyainrong block

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图 4 安多—聂荣地块西南缘韧性剪切带(观测点D53)⁴⁰Ar/³⁹Ar坪年龄与等时线年龄

Figure 4. ⁴⁰Ar/³⁹Ar plateau age and isochron age of the ductile shear belts at the southwest margin of the Ando-Nyainrong block(Site D53)

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图 5 安多—聂荣地块西北缘韧性剪切带(观测点D56)⁴⁰Ar/³⁹Ar坪年龄与等时线年龄

Figure 5. ⁴⁰Ar/³⁹Ar plateau age and isochron age of the ductile shear belts at the northwest margin of the Ando-Nyainrong block(Site D56)

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表 1 安多—聂荣地块韧性剪切变形测量结果与北东—南西向挤压构造应力场

Table 1. Results of ductile shear deformation analysis and the NE-SW direction compressional tectonic stress field in the Ando-Nyainrong block

点号	经度(E)	纬度(N)	数据量	σ₁(az°/pl°)	σ₂(az°/pl°)	σ₃(az°/pl°)	R
D20	92°20′01″	32°07′16″	19	333/41	085/22	196/39	0.7
D21	92°18′45″	32°07′29″	5	186/34	047/47	292/21	0.7
D22	92°17′44″	32°06′26″	5	153/29	248/08	353/58	0.2
D25	92°12′14″	32°03′23″	4	320/43	111/42	215/15	0.3
D28	92°04′05″	31°47′32″	4	NNE-SSW
D45	93°06′34″	31°50′10″	9	320/18	097/65	225/15	0.1
D53	91°42′06″	31°52′51″	7	244/24	137/33	002/46	0.8
D55	91°41′49″	32°06′05″	4	063/05	157/29	323/59	0.5
D56	91°42′45″	32°07′15″	7	100/17	209/45	355/39	0.5
D70	91°40′56″	32°02′05″	5	030/15	297/11	172/70	0.4
注：σ₁—最大主应力；σ₂—中间主应力；σ₃—最小主应力；az—倾伏向；pl—倾伏角；R=(σ₂-σ₃/σ₁-σ₃)

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表 2 安多—聂荣地块西南缘韧性剪切带(观测点D53)⁴⁰Ar/³⁹Ar坪年龄与等时线年龄

Table 2. ⁴⁰Ar/³⁹Ar plateau age and isochron age of the ductile shear belts at the southwest margin of the Ando-Nyainrong block(Site D53)

T/℃	(⁴⁰Ar/ ³⁹Ar) _m	⁽³⁶Ar/ ³⁹Ar) _m	(³⁷Ar ₀/ ³⁹Ar) _m	(³⁸Ar/ ³⁹Ar) _m	⁴⁰Ar/%	F	³⁹Ar/10 ^-14mol	³⁹Ar(Cum.)/%	Age/Ma	±1σ/Ma
D53-1钾长石 W=27.71 mg J=0.002684 Total age=161.0Ma
700	165.8118	0.1561	0.7508	0.0540	72.22	119.8151	0.06	0.33	503.0	5.9
800	31.5490	0.0041	0.0206	0.0137	96.14	30.3332	1.28	6.84	141.2	1.4
860	28.0541	0.0010	0.0474	0.0129	98.90	27.7466	0.80	10.93	129.6	1.3
920	28.3819	0.0031	0.1538	0.0141	96.81	27.4801	0.62	14.06	128.4	1.3
980	28.7767	0.0015	0.1156	0.0130	98.46	28.3349	0.35	15.83	132.2	1.4
1040	30.5556	0.0048	0.0293	0.0139	95.30	29.1211	0.64	19.07	135.8	1.4
1100	34.8159	0.0072	0.0410	0.0148	93.85	32.6757	1.03	24.32	151.6	1.5
1160	37.8379	0.0090	0.0237	0.0147	92.95	35.1694	1.65	32.70	162.7	1.6
1210	38.8774	0.0080	0.0170	0.0147	93.90	36.5066	3.23	49.13	168.6	1.6
1260	38.2769	0.0067	0.0052	0.0142	94.83	36.2989	6.82	83.80	167.7	1.6
1290	37.4411	0.0059	0.0204	0.0141	95.33	35.6945	2.62	97.10	165.0	1.6
1330	37.8766	0.0080	0.1179	0.0146	93.74	35.5089	0.43	99.27	164.2	1.7
1400	40.3533	0.0196	0.3614	0.0165	85.72	34.5995	0.14	100.00	160.2	2.4
D56-1黑云母 W=33.07 mg J=0.002735 Total age=165.6Ma
700	56.7666	0.1419	1.2378	0.0440	26.28	14.9359	0.06	0.37	72.2	5.2
760	36.0626	0.0190	0.1219	0.0169	84.48	30.4678	1.00	6.30	144.4	1.4
800	36.3997	0.0037	0.0783	0.0139	96.99	35.3058	1.61	15.86	166.3	1.6
840	36.1519	0.0021	0.0000	0.0133	98.24	35.5169	1.64	25.62	167.3	1.6
880	36.0022	0.0024	0.1252	0.0138	98.05	35.3049	1.15	32.45	166.3	1.6
920	36.0515	0.0017	0.0771	0.0134	98.59	35.5449	1.15	39.31	167.4	1.6
960	36.0165	0.0019	0.1006	0.0134	98.47	35.4710	1.13	46.01	167.0	1.6
1000	36.2395	0.0019	0.0167	0.0131	98.46	35.6825	1.13	52.75	168.0	1.6
1040	35.9673	0.0014	0.0470	0.0134	98.82	35.5425	2.20	65.84	167.4	1.6
1080	36.0125	0.0015	0.0312	0.0133	98.78	35.5726	2.63	81.46	167.5	1.6
1200	36.1565	0.0014	0.0076	0.0130	98.88	35.7507	2.96	99.05	168.3	1.6
1400	39.5904	0.0179	0.7467	0.0179	86.78	34.3776	0.16	100.00	162.1	2.3
注：表中下标m代表样品中测定的同位素比值，F=⁴⁰Ar^*/³⁹Ar, is the ratio of radiogenic Argon40 and Argon39

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