华北临汾盆地中部柴庄上新世-更新世剖面沉积学特征及其构造意义

陈兴强; 施炜; 胡健民; 董树文

华北临汾盆地中部柴庄上新世-更新世剖面沉积学特征及其构造意义

陈兴强^{1, 2,},
施炜¹,
胡健民¹,
董树文³

1.
中国地质科学院地质力学研究所, 北京 100081
2.
北京大学地球与空间科学学院, 北京 100871
3.
南京大学地球科学与工程学院, 南京 210023

基金项目:

中国地质调查局地质调查项目“特殊地质地貌区填图试点” DD20160060

中国地质调查局地质调查项目“主要活动构造带关键地段区域质专项调查” 1212011120099

国家自然科学基金项目“鄂尔多斯地块周缘新生代断陷盆地形成机理” 41672203

详细信息

作者简介:
陈兴强(1986-), 男, 博士研究生, 构造地质学专业, 主要从事新生代沉积盆地演化过程研究。E-mail:cxq123111@163.com

中图分类号: P512.2;P546
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出版历程
- 收稿日期: 2016-09-16
- 刊出日期: 2016-12-01

SEDIMENTATION OF THE PLIOCENE-PLEISTOCENE CHAIZHUANG SECTION IN THE CENTRAL OF LINFEN BASIN, NORTH CHINA AND ITS TECTONIC SIGNIFICANCE

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth and Space Science, Peking University, Beijing 100871, China
3.
School of Earth Science and Engineering, Nanjing University, Nanjing 210093, China

摘要

摘要: 临汾盆地位于华北克拉通汾渭地堑系中南部，是典型的受控于北东-南西向和近东西向正断层的晚新生代断陷盆地。沉积相、古水流和重矿物综合分析表明，盆地中部的柴庄新生界剖面除顶部的风成黄土之外，可以划分为3个岩性段，分别具有不同的物源，反映了不同时期的构造背景。第一岩性段为上新统（5.0~2.6 Ma），冲积扇和风成红黏土沉积，冲积扇碎屑物源为盆地周缘的灰岩等沉积岩类；第二岩性段为更新统下部（2.6~1.0 Ma），三角洲相沉积，沉积物来自盆地南缘中条山北部和东缘太行山西部的太古宇-下元古界的花岗片麻岩和片麻岩、上元古界-古生界的碳酸盐岩、中生界的陆源碎屑岩及少量不同时代的花岗岩；第三段为更新统中上部（ < 1.0 Ma），河流相沉积，主要物源为盆地北东缘太行山的花岗岩类、少量沉积岩和变质岩。结合区域应力演化过程认为，距今5.0~2.6 Ma期间，受北西-南东向伸展作用影响，北东-南西向正断层为盆地的主控断层；距今2.6~1.0 Ma时期，主要受到北东-南西伸展应力的影响，近东西向断层开始活动；距今1.0 Ma以来，沉积环境由三角洲和湖泊相转为河流相沉积，指示盆地发育的减弱，可能与后一期伸展应力的减弱有关。上述结果表明，受青藏高原向北东扩展的影响，汾渭地堑系至少经历了中新世晚期-上新世早期（>5 Ma）、2.6 Ma和1.0 Ma等主要构造转换时代。
- 临汾盆地 /
- 沉积相 /
- 物源 /
- 新构造 /
- 青藏高原
Abstract: Linfen Basin is located in middle-southern part of the Fenwei Graben systems, North China Craton. As a late Cenozoic rift basin, it was defined by the northeast-striking and east-striking normal faults. Comprehensive constraints of sedimentary facies and provenance of the Chaizhuang section in the middle part of the basin indicating that the section can be divided into three units with different source areas, with some loess on the top of the section. This may provide important clues for exploring the tectonic setting of the basin evolution. Unit 1 in Pliocene (5~2.6 Ma) was deposited in alluvial fan and eolian environment with the nearby sedimentary rocks (i.e. limestone) to be the main source rocks. Unit 2 in the lower part of the Pleistocene (2.6~1.0 Ma) was deposited in a delta environment with mixed source rocks shed from Taihang Mountains and Zhongtiao Mountains on the eastern and southeastern of the basin, which include the Archean-Palaeoproterozoic granitic gneiss and gneiss, Neoproterozoic-Paleozoic carbonatite, Mesozoic terrigenous clastic rocks and some granitoids. Unit 3 in the upper part of the Pleistocene ( < 1.0 Ma) was deposited in a fluvial environment with the acidic magmatic rocks derived from the Taihang Mountains on the northeastern of the basin. Combined with the late Cenozoic regional regime evolution of the Shanxi Graben, we proposed that the northeast-striking normal faults were strongly active in Pliocene and influenced by the transtensional stress regime under NW-SE extension. The east-striking faults seem to be active in early Pleistocene (2.6~1.0 Ma) and were influenced by the NE-SW extension. From 1.0 Ma, the fluvial replaced the delta and lacustrine sedimentary environments. This indicates that the basin evolution is not as strong as in early Pleistocene which may be a result of the weakening of the extension. All these clues indicate that the main tectonic transition ages in Fenwei Graben systems influenced by the Tibetan in Pliocene-Pleistocene may include Late Miocene-early Pliocene (5.0 Ma), 2.6 Ma and 1.0 Ma.
- Linfen Basin /
- sedimentary facies /
- Provenance /
- neotectonic /
- Tibetan Plateau

HTML全文

图 1 临汾盆地大地构造位置图^[8](a), 构造纲要图^[14](b)及区域地质简图(c)

Figure 1. A map showing tectonic location, structure outline and regional geology of the Linfen Basin

下载: 全尺寸图片幻灯片

图 2 临汾盆地柴庄剖面与LK10孔^[13]岩相图对比

Figure 2. Lithofacies comparison between Chaizhuang section and LK10 core in the Linfen Basin

下载: 全尺寸图片幻灯片

图 3 柴庄新生界剖面典型沉积学野外露头照片

a—块状沉积的砾石层, 颗粒支撑; b—块状沉积的红黏土及砂岩; c—含泥砾的粗砂层及板状斜层理砂岩; d—下部为质地均一而纯净的砂体, 上部为含炭屑灰黄色、灰绿色粉砂和黏土沉积; e—向上变粗的河流相沉积旋回, 照片下部和顶部(含贝壳化石)为含细砾粗砂岩, 向上为发育低角度斜层理中、细砂岩和块状层理的粉砂岩; f—板状斜层理砂岩; g—发育在河流相砂岩中哺乳动物化石

Figure 3. The field outcrop photos of the typical Cenozoic sedimentation in the Chaizhuang section

下载: 全尺寸图片幻灯片

图 4 柴庄剖面重矿物含量(a)及重矿物组合含量(b)统计图

Figure 4. Statistical maps showing contents of detrital heavy minerals and their combination in Chaizhuang section

下载: 全尺寸图片幻灯片

参考文献(30)

[1]	Zhang Y, Vergely P, Mercier J L, et al. Kinematic history and changes in the tectonic stress regime during the Cenozoic along the Qinling and southern Tanlu fault zones[J]. Acta Geologica Sinica:English Edition, 1999, 73(3):264~274. doi: 10.1111/acgs.1999.73.issue-3
[2]	邓起东, 程绍平, 闵伟, 等.鄂尔多斯块体新生代构造活动和动力学的讨论[J].地质力学学报, 1999, 5(3):13~21. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=19990333&flag=1 DENG Qi-dong, CHENG Shao-ping, MIN wei, et al. Discussion on Cenozoic tectonics and dynamics of Ordos Block[J]. Journal of Geomechanics, 1999, 5(3):13~21. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=19990333&flag=1
[3]	Zhang Y, Ma Y, Yang N, et al. Cenozoic extensional stress evolution in North China[J]. Journal of Geodynamics, 2003, 36(5):591~613. doi: 10.1016/j.jog.2003.08.001
[4]	张培震, 郑德文, 尹功明, 等.有关青藏高原东北缘晚新生代扩展与隆升的讨论[J].第四纪研究, 2006, 26(1):5~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601001.htm ZHANG Pei-zhen, ZHENG De-wen, YIN Gong-ming, et al. Discussion on late Cenozoic growth and rise of northeastern margin of the Tibetan Plateau[J]. Quaternary Sciences, 2006, 26(1):5~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601001.htm
[5]	张岳桥, 廖昌珍, 施炜, 等.鄂尔多斯盆地周边地带新构造演化及其区域动力学背景[J].高校地质学报, 2006, 12(3):285~297. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200603002.htm ZHANG Yue-qiao, LIAO Chang-zhen, SHI Wei, et al. Neotectonic evolution of the peripheral zones of the Ordos Basin and geodynamic setting[J]. Geological Journal of China Universities, 2006, 12(3):285~297. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200603002.htm
[6]	Yin A. Cenozoic tectonic evolution of Asia:A preliminary synthesis[J]. Tectonophysics, 2010, 488(1/4):293~325. http://www.sciencedirect.com/science/article/pii/S0040195109003217
[7]	Chen X, Chi Z, Dong S, et al. Late Cenozoic sedimentation of Nihewan Basin, central North China and its tectonic significance[J]. Journal of Asian Earth Sciences, 2015, 114:242~257. doi: 10.1016/j.jseaes.2015.06.020
[8]	Shi W, Cen M, Chen L, et al. Evolution of the late Cenozoic tectonic stress regime in the Shanxi Rift, central North China Plate inferred from new fault kinematic analysis[J]. Journal of Asian Earth Sciences, 2015, 114:54~72. doi: 10.1016/j.jseaes.2015.04.044
[9]	Peltzer G, Tapponnier P, Zhang Z, et al. Neogene and Quaternary faulting in and along the Qinling Shan[J]. Nature, 1985, 317(6037):500~505. doi: 10.1038/317500a0
[10]	胡小猛, 杨景春.临汾盆地中更新世中晚期以来的演化历史及成因分析[J].上海师范大学学报:自然科学版, 2001, 30(3):72~76. http://www.cnki.com.cn/Article/CJFDTOTAL-SHDZ200103014.htm HU Xiao-meng, YANG Jing-chun. The evolution and its contributing factors of Linfen Basin since middle Quaternary[J]. Journal of Shanghai Teachers University:Natural Sciences, 2001, 30(3):72~76. http://www.cnki.com.cn/Article/CJFDTOTAL-SHDZ200103014.htm
[11]	Hu X, Li Y, Yang J. Quaternary paleolake development in the Fen River basin, North China[J]. Geomorphology. 2005, 65(1/2):1~13. http://www.sciencedirect.com/science/article/pii/S0169555X0400162X
[12]	胡小猛, 杨景春.临汾盆地末次间冰期以来地貌演化的构造和气候响应[J].地质力学学报. 2001, 7(2):176~180. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20010227&flag=1 HU Xiao-meng, YANG Jing-chun. The response of the development of Fen River to Neotectonic movement and paleoclimate changes since last Non-Glaciation stage[J]. Journal of Geomechanics, 2001, 7(2):176~180. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20010227&flag=1
[13]	莫多闻.山西临汾盆地晚新生代环境演变研究[J].北京大学学报:自然科学版, 1991, 27(6):738~746. http://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ199106015.htm MO Duo-wen. The study on the late Cenozoic environment change of Linfen Basin, Shanxi Province[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 1991, 27(6):738~746. http://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ199106015.htm
[14]	邓起东, 苏宗正, 王挺梅, 等. 临汾盆地晚第四纪沉积与最新构造运动[C]//山西临汾地震研究与系统减灾. 北京: 地震出版社, 1993: 111~129. DENG Qi-dong, SU Zong-zheng, WANG Ting-mei, et al. Late Quaternary sedimentary and tectonic movement of Linfen Basin[C]//Linfen Earthquake Research and Systematic Disaster Reduction in Shanxi. Beijing:Seismological Press, 1993:111~129.
[15]	王乃梁, 杨景春, 夏正楷.山西地堑系新生代沉积与构造地貌[M].北京:科学出版社, 1996. WANG Nai-liang, YANG Jing-chun, XIA Zheng-kai. Cenozoic sedimentation and tectonic geomorphology of the Shanxi Grabens[M]. Beijing:Science Press, 1996.
[16]	王成善, 李祥辉.沉积盆地分析原理与方法[M].北京:高等教育出版社, 2003. WANG Cheng-shan, LI Xiang-hui. Sedimentary basin:From principles to analysis[M]. Beijing:Higher Education Press, 2003.
[17]	Molnar P. Mio-Pliocene growth of the Tibetan Plateau and evolution of East Asian climate[J]. Palaeontologia Electronica. 2005.
[18]	张培震, 张会平, 郑文俊, 等.东亚大陆新生代构造演化[J].地震地质, 2014, 36(3):574~585. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201403004.htm ZHANG Pei-zhen, ZHANG Hui-ping, ZHENG Wen-jun, et al. Cenozoic tectonic evolution of continental eastern Asia[J]. Seismology and Geology, 2014, 36(3):574~585. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201403004.htm
[19]	Liu J, Zhang P, Lease R O, et al. Eocene onset and late Miocene acceleration of Cenozoic intracontinental extension in the North Qinling range-Weihe graben:Insights from apatite fission track thermochronology[J]. Tectonophysics, 2013, 584:281~296. doi: 10.1016/j.tecto.2012.01.025
[20]	Liu J, Zhang P, Zheng D, et al. Pattern and timing of late Cenozoic rapid exhumation and uplift of the Helan Mountain, China[J]. Science China:Earth Sciences, 2010, 53(3):345~355. doi: 10.1007/s11430-010-0016-0
[21]	Song Y, Fang X, Torii M, et al. Late Neogene rock magnetic record of climatic variation from Chinese eolian sediments related to uplift of the Tibetan Plateau[J]. Journal of Asian Earth Sciences, 2007, 30(2):324~332. doi: 10.1016/j.jseaes.2006.10.004
[22]	施雅风, 李吉均, 李炳元, 等.晚新生代青藏高原的隆升与东亚环境变化[J].地理学报, 1999, 54(1):12~22. http://www.cnki.com.cn/Article/CJFDTOTAL-DLXB901.001.htm SHI Ya-feng, LI Ji-jun, LI Bing-yuan, et al. Uplift of the Qinghai-Xizang (Tibetan) Plateau and east Asia environmental change during late Cenozoic[J]. Acta Geographica Sinica, 1999, 54(1):12~22. http://www.cnki.com.cn/Article/CJFDTOTAL-DLXB901.001.htm
[23]	李吉均, 方小敏, 马海洲, 等.晚新生代黄河上游地貌演化与青藏高原隆起[J].中国科学D辑:地球科学, 1996, (4):316~322. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199604004.htm LI Ji-jun, FANG Xiao-min, MA Hai-zhou, et al. Geomorpological evolution in the upper reaches of the Yellow River during the Iate Cenozoic[J]. Science in China Series D:Earth Sciences, 1996, (4):316~322. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199604004.htm
[24]	李吉均, 文世宣, 张青松, 等.青藏高原隆起的时代, 幅度和形式的探讨[J].中国科学, 1979, 6:608~616. http://www.cnki.com.cn/Article/CJFDTOTAL-JAXK197906008.htm LI Ji-jun, WEN Shi-xuan, ZHANG Qing-song, et al. The discussion of the uplift era, amplitude and form of the Tibet Plateau[J]. Science in China, 1979, 6:608~616. http://www.cnki.com.cn/Article/CJFDTOTAL-JAXK197906008.htm
[25]	申旭辉, 田勤俭, 丁国瑜, 等.宁夏贺家口子地区晚新生代地层序列及其构造意义[J].中国地震, 2001, 17(2):156~166. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD200102004.htm SHEN Xu-hui, TIAN Qin-jian, DING Guo-yu, et al. The late Cenozoic stratigraphic sequence and its implication to tectonic evolution, Hejiakouzi area, Ningxia Hui Autonomous Region[J]. Earthquake Research in China, 2001, 17(2):156~166. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD200102004.htm
[26]	Sun J. Long-term fluvial archives in the Fen Wei Graben, central China, and their bearing on the tectonic history of the India-Asia collision system during the Quaternary[J]. Quaternary Science Reviews, 2005, 24(10/11):1279~1286.
[27]	Su H, Wang J, Pan B, et al. Sequences and genesis of the Yellow River terraces from Sanmen Gorge to Kouma[J]. Journal of Geographical Sciences, 2009, 19(3):351~358. doi: 10.1007/s11442-009-0351-2
[28]	Pan B, Wang J, Gao H, et al. Terrace dating as an archive of the run-through of the Sanmen Gorges[J]. Progress in Natural Science, 2005, 15(12):1096~1103. doi: 10.1080/10020070512331343191
[29]	Pan B, Wang J, Gao H, et al. Paleomagnetic dating of the topmost terrace in Kouma, Henan and its indication to the Yellow River's running through SanmenGorges[J]. Chinese Science Bulletin, 2005, 50(7):657~664. doi: 10.1360/03wd0290
[30]	陈兴强, 迟振卿, 闫臻, 等.华北泥河湾盆地郝家台地区的沉积相组合特征:以台儿沟东剖面为例[J].地学前缘, 2012, 19(4):227~238. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201204025.htm CHEN Xing-qiang, CHI Zhen-qing, YAN Zhen, et al. Features of sedimentary facies of the Nihewan Basin in North China:An example from the Eastern Taiergou section[J]. Earth Science Frontiers, 2012, 19(4):227~238. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201204025.htm