北京房山地区太平山褶皱的变形特征和形成时代:华北克拉通早白垩世挤压构造的意义

舒坦; 续海金; 章军锋; 刘强

doi:10.3799/dqkx.2018.119

北京房山地区太平山褶皱的变形特征和形成时代:华北克拉通早白垩世挤压构造的意义

doi: 10.3799/dqkx.2018.119

中国地质大学地球科学学院, 湖北武汉 430074

基金项目:

国家自然科学基金项目 41772054

国家自然科学基金项目 41572039

详细信息

作者简介:
舒坦(1991-), 男, 在读博士研究生, 主要从事构造地质学研究

通讯作者:
续海金

中图分类号: P54
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出版历程
- 收稿日期: 2019-01-06
- 刊出日期: 2019-05-15

Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton

School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

摘要

摘要: 北京西山地区广泛发育轴向近E-W向的褶皱，对理解华北克拉通东部构造演化至关重要，但目前对其形成时代和构造动力学背景却没有明确的认识.北京房山地区的太平山褶皱是轴向近E-W向褶皱的典型代表.通过精细的野外构造观察和构造年代学研究，确定太平山褶皱的空间展布特征和构造样式，厘定构造变形的时代，为该区乃至华北克拉通东部的构造演化提供重要依据.通过详细的野外构造观察和系统的β图解研究，表明太平山褶皱由直立倾伏背斜和斜歪倾伏向斜构成.通过对早期卷入褶皱变形的煌斑岩席和晚期切层侵入褶皱的闪长玢岩脉进行锆石U-Pb定年，得到煌斑岩席和闪长玢岩脉的形成时代分别为147.2±2.4 Ma和129.0±3.2 Ma，表明太平山褶皱的形成时代为燕山运动B幕.另外，北京西山地区还存在NW-SE向的伸展构造样式.代表本区NW-SE向伸展的房山穹窿（约136 Ma）晚于N-S向挤压构造，侵入切割太平山褶皱，塑造了研究区现今主体构造格架，进一步限定太平山褶皱的形成时代为147~136 Ma.因此，研究区轴向近E-W向的褶皱为早白垩世近N-S向挤压构造的产物；N-S向挤压和NW-SE向伸展的构造样式，为华北克拉通中生代构造体制的转换和动力学背景提供关键依据.
- 构造变形 /
- 变形时代 /
- 构造体制 /
- 北京西山 /
- 华北克拉通 /
- 构造地质
Abstract: The folds with near E-W-trending fold axis are widely developed in the Western Hills of Beijing, which are very important for understanding the tectonic evolution of the eastern part of North China craton (NCC). However, their deformation age and tectonic dynamic background are poorly understood. Taipingshan folds in the Fangshan area, Beijing, are typical folds with near E-W axial orientation. The detailed field structure observation and tectonic geochronology were carried out to determine the spatial distribution characteristics and tectonic style of Taipingshan folds and their deformation age. The detailed field structure observation and systematic β-diagrams study show that the Taipingshan folds consist of an upright capsized anticline and an inclined capsized syncline. A deformed lamprophyre sheet which is earlier than the folds structure gives a weighted zircon U-Pb age of 147.2±2.4 Ma, and the later porphyrite dyke that cuts strata of the folds gives a weighted zircon U-Pb age of 129.0±3.2 Ma, suggesting that the deformation time of the Taipingshan folds is between ca. 147 and 129 Ma, belonging to phase B of "Yanshanian movement". In addition, the extensional structure with NW-SE extensional direction is also developed in the Western Hills of Beijing. Fangshan dome (about 136 Ma), which is a typical product of the extensional tectonic, intruded into and cut the Taipingshan folds, further limiting the deformation age of the Taipingshan folds ranges from ca. 147 to 136 Ma. Thus, the folds with E-W-trending fold axis in the studied area are products of nearly N-S compressional tectonics in Early Cretaceous. The tectonic regime transformation from N-S compressional to NW-SE extensional tectonics provides a key understanding on tectonic dynamics of the eastern part of NCC in Late Mesozoic.
- tectonic deformation /
- deformation time /
- tectonic regime /
- Western Hills of Beijing /
- North China craton /
- tectonics

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图 1 华北克拉通地质简图(a)和北京西山南部区域地质构造略图(b)

图a据Wang et al.(2010)修改; 图b据赵温霞(2003)修改.1.第四系; 2.白垩系; 3.侏罗系; 4.三叠系至石炭系; 5.寒武系-奥陶系; 6.新元古界青白口系; 7.中元古界蓟县系; 8.中元古界长城系; 9.太古宇官地杂岩; 10.房山花岗闪长岩体; 11.背斜轴迹; 12.向斜轴迹; 13.拆离断层; 14.逆断层产状(°); 15.正断层产状(°); 16.地质界线; 17.平行不整合及角度不整合; 18.面理产状(°); 19.城镇及居民点; 20.剖面线

Fig. 1. Geological sketch map of North China craton (a) and regional structural and geological sketch map of the southern part of the Western Hills of Beijing (b)

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图 2 房山地区太平山-官地地层实测剖面

剖面A-A’见图 1b

Fig. 2. Measured stratigraphic section from Taipingshan to Guandi in the Fangshan area

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图 3 太平山褶皱的出露特征

a.太平山褶皱三维示意; b.164背斜的β图解; c.太平山向斜的β图解; d.164背斜平行于轴面剖面; e.164背斜直立剖面

Fig. 3. Exposed features of Taipingshan fold

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图 4 闪长玢岩脉侵入至马家沟组灰岩(a)和风化的闪长玢岩(b)

Fig. 4. The dioritic porphyrite dyke intruded into limestone of Majiagou Formation (O₂m) (a) and weathered dioritic porphyrite (b)

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图 5 164背斜布丁状煌斑岩脉显微照片

a.煌斑结构, 斑晶主要为黑云母和斜长石; b.煌斑岩侵入时捕获围岩灰岩

Fig. 5. Photomicrographs of the pudding lamprophyre dyke in the 164-anticline

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图 6 煌斑岩(a)和闪长玢岩(b)锆石阴极发光图像及LA-ICP-MS测年分析点位

Fig. 6. Representative cathodoluminescence (CL) images of zircon grains with ²⁰⁶Pb/²³⁸U age (Ma) from 164-anticline lamprophyre (a) and diorite porphyrite (b) from Daliyanshan

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图 7 煌斑岩(a)和闪长玢岩(b)LA-ICP-MS锆石U-Pb年龄谐和图

Fig. 7. Zircon U-Pb concordia diagrams for lamprophyre (a) and diorite porphyrite (b)

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图 8 黄院村采石场-小东沟地层信手剖面

剖面B-B’见图 1b

Fig. 8. Draft stratigraphic section of Huangyuan quarry-Xiaodonggou

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图 9 太平山褶皱的形成和演化

a.地层沉积阶段；b.大约147 Ma，煌斑岩呈席状侵入至马家沟组灰岩中；c.147~136 Ma，近N-S的挤压形成E-W向太平山褶皱；d.大约136 Ma，房山岩体底侵形成穹窿构造并造成太平山向斜北翼陡倾、地层缺失减薄，此后在129 Ma，闪长玢岩脉形成并切层侵入至马家沟组灰岩中

Fig. 9. The formation and evolution of Taipingshan fold

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表 1 房山地区太平山煌斑岩和闪长玢岩LA-ICP-MS锆石U-Pb测年分析结果

Table 1. LA-ICP-MS zircon U-Pb isotope data for lamprophyre and diorite porphyrite from Taipingshan, Fangshan area

点号	Pb(10^-6)	Th(10^-6)	U(10^-6)	Th/U	同位素比值						年龄(Ma)
点号	Pb(10^-6)	Th(10^-6)	U(10^-6)	Th/U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
煌斑岩(ZKD12-1)，n=7
1.1	92	904	1 584	0.570	0.047 7	0.002 5	0.149 8	0.008 0	0.022 6	0.000 3	83.4	127.8	142	7.0	144	2.0
2.1	222	2 740	1 439	1.900	0.049 0	0.002 5	0.154 7	0.007 9	0.022 8	0.000 3	150.0	116.0	146	7.0	146	2.0
3.1	14	448	447	1.000	0.055 2	0.003 4	0.172 9	0.010 2	0.022 9	0.000 3	420.0	137.0	162	8.9	146	2.1
4.1	8	277	244	1.130	0.055 1	0.003 5	0.175 5	0.010 8	0.023 1	0.000 5	417.0	144.0	164	9.3	147	2.9
5.1	31	895	1 008	0.890	0.057 1	0.002 6	0.184 3	0.008 0	0.023 2	0.000 3	494.0	100.0	172	6.9	148	1.8
6.1	21	693	653	1.060	0.046 2	0.002 3	0.149 9	0.007 2	0.023 5	0.000 3	5.7	115.0	142	6.4	150	2.1
7.1	12	547	302	1.810	0.054 1	0.003 3	0.177 3	0.010 6	0.023 9	0.000 4	376.0	137.0	166	9.1	152	2.4
闪长玢岩(15ZKD-DLYS)，n=9
1.1	51.2	432.1	456.9	0.946	0.050 512	0.003 983	0.147 009	0.011 528	0.021 042	0.000 342	220.4	178.7	139.3	10.2	134.2	2.2
2.1	88.3	800.3	545.0	1.469	0.054 716	0.003 914	0.162 340	0.011 425	0.021 547	0.000 317	466.7	161.1	152.7	10.0	137.4	2.0
3.1	379.0	3 635.6	1 961.1	1.854	0.048 056	0.001 801	0.129 463	0.004 815	0.019 552	0.000 190	101.9	88.9	123.6	4.3	124.8	1.2
4.1	66.3	604.3	461.0	1.311	0.061 834	0.004 928	0.159 428	0.010 747	0.019 808	0.000 367	733.3	172.2	150.2	9.4	126.4	2.3
5.1	120.7	1 129.2	729.3	1.548	0.054 523	0.003 317	0.147 510	0.008 710	0.019 927	0.000 364	394.5	137.0	139.7	7.7	127.2	2.3
6.1	36.2	314.8	358.8	0.877	0.052 998	0.004 461	0.152 499	0.013 333	0.020 763	0.000 346	327.8	192.6	144.1	11.7	132.5	2.2
8.1	151.3	1 351.9	888.2	1.522	0.053 070	0.003 437	0.149 219	0.009 312	0.020 564	0.000 267	331.5	148.1	141.2	8.2	131.2	1.7
9.1	466.9	4 612.8	1 998.7	2.308	0.049 243	0.002 286	0.138 045	0.006 256	0.020 281	0.000 204	166.8	104.6	131.3	5.6	129.4	1.3
10.1	145.0	1 441.7	969.2	1.487	0.047 417	0.002 297	0.129 167	0.006 175	0.019 675	0.000 250	77.9	111.1	123.3	5.6	125.6	1.6

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