地球科学进展 ›› 2013, Vol. 28 ›› Issue (10): 1126 -1135. doi: 10.11867/j.issn.1001-8166.2013.10.1126

综述与评述 上一篇    下一篇

渭河盆地新生代地层与沉积演化研究: 现状和问题
王斌 1, 郑洪波 2, *, 王平 2, 何忠 3   
  1. 1.南京大学地球科学与工程学院, 江苏 南京 210093; 
    2.南京师范大学地理科学学院, 江苏 南京210046; 
    3. 西北农林科技大学水土保持研究所, 陕西 杨凌 712100
  • 收稿日期:2013-06-13 出版日期:2013-10-10
  • 通讯作者: 郑洪波(1965-), 男, 山东乳山人, 教授, 主要从事第四纪地质与过去全球变化研究. E-mail: zhenghb@njnu.edu.cn
  • 基金资助:

    中国科学院战略性先导科技专项(B类)“青藏高原多层圈相互作用及其资源环境效应”(编号:XDB03020300)资助.

The Cenozoic Strata and Depositional Evolution of Weihe Basin: Progresses and Problems

Wang Bin 1, Zheng Hongbo 2, Wang Ping 2, He Zhong 3   

  1. 1. School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China; 
    2. School of Geography Science, Nanjing Normal University, Nanjing 210046, China; 
    3. Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China
  • Received:2013-06-13 Online:2013-10-10 Published:2013-10-10

在前人划分基础上对渭河盆地新生代地层进行了重新梳理和部分修订, 将红河组、白鹿塬组、冷水沟组、寇家村组、灞河组、蓝田组、三门组等区域地层单位及第四纪黄土—古土壤与《中国区域年代地层表》进行了对照:把原属于蓝田组底部的砾岩层划入灞河组;对三门组的概念和内涵进行了界定, 认为其和蓝田组属于同期异相沉积而不存在上下关系;主张取消“张家坡组”和“游河组”并将其归入三门组。分析了渭河盆地始新世以来的构造张裂和沉积演化历史, 认为始新世和晚中新世是其发育演化最重要的2个阶段, 在时间和动力上与秦岭造山带的隆升以及鄂尔多斯高原的演化具有协同一致性。

On the basis of the previous stratigraphic research, the Cenozoic strata in the Weihe Basin have been recognized and partially revised. The main regional stratigraphic units in the Weihe Basin are compared with the “China Regional Chronostratigraphic (Geo-chronologic) Scale”, including the Honghe Formation, the Bauluyuan Formation, and the Lengshuigou Formation, the Koujiacun Formation, the Bahe Formation, the Lantian Formation, the Sanmen Formation and the Quaternary loesspaleosol. We found that the conglomerate at the bottom of Lantian Formation should be thought as the upper part of the Bahe Formation. The Sanmen Formation is defined more clearly that it has no vertical relationship with the Lantian Formation. These two formations are the contemporaneous heterotopic facies within the same deposition period, but over different environments, and they have never been found in one section in the Weihe Basin. The “Zhangjiapo Formation” and the “Youhe Formation” were wrongly founded and placed in time before, they should be concealed and belong to the “Sanmen Formation”. The tectonic rifting and sedimentary evolution of the Weihe Basin has been analyzed and reviewed, and the Eocene and late Miocene are found as the two most important developmental stages of the Weihe Basin during the Cenozoic era. The Weihe basin is synergistic and related to the uplifting of the Qinling Mountains and the evolution of the Ordos Plateau in time and motivation.

中图分类号: 

[1]Molnar P, Tapponnier P. Cenozoic Tectonics of Asia: Effects of a continental collision[J]. Science, 1975, 189(4 201): 419-426.
[2]Searle M, Windley B, Coward M, et al. The closing of the Tethys and the tectonics of the Himalaya[J]. Geological Society of American Bulletin, 1987, 98: 678-701.
[3]Tapponnier P, Peltzer G, Le Dain A, et al. Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine[J]. Geology, 1982, 10(12): 611-616.
[4]Peltzer G, Tapponnier P, Zhang Z, et al. Neogene and Quaternary faulting in and along the Qinling Shan[J]. Nature, 1985, 317: 500-505.
[5]Mattauer M, Matte P, Malavieille J, et al. Tectonics of the Qinling Belt: Build-up and evolution of eastern Asia[J]. Nature, 1985, 317: 496-500.
[6]Sun J. Long-term fluvial archives in the Fenwei 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: 1 279-1 286.
[7]Zhang Bosheng. The bearing of block faulting to stream development on both sides of the Qinling Ranges[J]. Acta Geological Sinica, 1964, 44(4): 405-417.[张伯声. 在块断构造的基础上说明秦岭两侧河流的发育[J]. 地质学报, 1964, 44(4): 405-417.]
[8]Wang Cuncheng. On the Weihe Graben[J]. Acta Geological Sinica, 1965, 45(2): 153-164.[王存诚. 论渭河地堑[J]. 地质学报, 1965, 45(2): 153-164.]
[9]Wang J. The Fenwei rift and its recent periodic activity[J]. Tectonophysics, 1987, 133: 257-275.]
[10]Cui Shengqin, Li Jinrong. Comparative tectonic analysis of Fen-Wei Graben and Baikal Rift System[J]. Bulletin of the Chinese Academy of Geological Sciences, 1986, 15: 21-31.[崔盛芹, 李锦蓉. 汾渭地堑与贝加尔裂谷系的比较构造分析[J]. 中国地质科学院院报, 1986, 15: 21-31.]
[11]Hu Mengchun. The relationship between the tectonic landforms and structures in the Weihe River Basin[J]. Geographical Research, 1989, 8(4): 56-64.[胡孟春. 渭河盆地的地质构造与构造地貌类型[J]. 地理研究, 1989, 8(4): 56-64.]
[12]Han Hengyue, Mi Fengshou, Liu Haiyun, et al. Geomorphological structure in the Weihe Basin and Neotectonic movement[J]. Journal of Seismologic Research, 2001, 24(3): 251-257.[韩恒悦, 米丰收, 刘海云, 等.渭河盆地带地貌结构与新构造运动[J]. 地震研究, 2001, 24(3): 251-257.]
[13]Peng Jianbing, Zhang Jun, Su Shengrui, et al. Active Faults and Geological Hazards in Weihe Basin[M]. Xi’an: Northwest University Press, 1992.[彭建兵, 张骏, 苏生瑞, 等. 渭河盆地活断裂与地质灾害[M]. 西安: 西北大学出版社, 1992.]
[14]Yang Zhongjian, Pei Wenzhong. On the Cenozoic geology between Luoyang and Sian[J]. Bulletin of the Geological Society of China, 1933, 13: 73-90.[杨钟健, 裴文中. 洛阳西安间之新生代地质[J]. 中国地质学会志, 1933, 13: 73-90.]
[15]Yang Zhongjian. Historical review about the Sanmen Formation[J]. Journal of Geological Review, 1936, 1(3): 323-330.[杨钟健. 三门系之历史的检讨[J]. 地质论评, 1936, 1(3): 323-330.]
[16]Liu Dongsheng, Ding Menglin, Gao Fuqing. Cenozoic stratigraphic sections between Xi’an and Lantian[J]. Geology Science, 1960, 4: 199-208.[刘东生, 丁梦麟, 高福清. 西安蓝田间新生界地层剖面[J]. 地质科学, 1960, 4: 199-208.]
[17]Wang Pinxian, Wang Naiwen, Bao Jinsong. Discovery of the Cenozoic foraminiferal in the Fen-Wei Basin and its significance[J]. Geological Review, 1982, 28(2): 93-100.[汪品先, 王乃文, 鲍金松. 汾渭盆地新生代有孔虫的发现及意义[J]. 地质论评, 1982, 28(2): 93-100.]
[18]Shaanxi Bureau of Geology and Mineral Resources. Regional Geology of Shaanxi Province[M]. Beijing: Geological Publishing House, 1989.[陕西地质矿产局. 陕西省区域地质志[M]. 北京: 地质出版社, 1989.]
[19]Porter S, An Z, Zheng H. Cyclic quaternary alluviation and terracing in a Nonglaciated drainage basin on the north flank of the Qinling Shan, central China[J]. Quaternary Research, 1992, 38: 157-169.
[20]Seismological Bureau of Shaanxi. Active Fault Zone in the North Margin of Qinling Mountains[M]. Beijing: Seismological Press, 1996.[陕西省地震局. 秦岭北缘活动断裂带[M]. 北京: 地震出版社, 1996.]
[21]Wang Jianqiang. Mesozoic-Cenozoic Basin Evolution-Reforming and Basin-Mountain Couping in Southern Ordos Basin[D]. Xi’an: Northwest University, 2010.[王建强.鄂尔多斯盆地南部中新生代演化—改造及盆山耦合关系[D]. 西安: 西北大学, 2010.]
[22]Zhang Hongwei, Deng Qidong. A study on the mechanism of the asymmetry basin—A case of the Weihe Basin[J]. Earthquake Research in China, 1992, 8(1): 26-35.[张宏卫, 邓起东. 不对称盆地形成机制探讨——以渭河盆地为例[J]. 中国地震, 1992, 8(1): 26-35.]
[23]Xue Xiangxu. An early Pleistocene mammalian fauna and its stratigraphy of the River You, Weinan, Shensi[J]. Vertebrata Palasiatica, 1981, 19(1): 35-44.[薛祥煦. 陕西渭南—早更新世哺乳动物群及其层位[J]. 古脊椎动物与古人类, 1981, 19(1): 35-44.]
[24]Xue Xiangxu, Zhang Yunxiang. The uplift stages and amplitudes of the Qinling Mountains by analysis the distribution and character of the fossils found in the mountains[J]. Geological Review, 1996, 42(1): 30-36.[薛祥煦, 张云翔. 从生物化石的性质和分布分析秦岭上升的阶段性与幅度[J]. 地质论评, 1996, 42(1): 30-36.]
[25]Xue Xiangxu, Li Wenhou, Liu Linyu. The northward shift of Weihe River and the uplift of Qinling Mountains[J]. Journal of Northwest University (Natural Science Edition), 2002, 32(5): 451-454.[薛祥煦, 李文厚, 刘林玉. 渭河北迁与秦岭抬升[J]. 西北大学学报:自然科学版, 2002, 32(5): 451-454.]
[26]Zhang Y, Ma Y, Yang N, et al. Cenozoic extensional stress evolution in North China[J]. Journal of Geodynamics, 2003, 36: 591-613.
[27]Zhang Yuping, Huang Wanbo, Tang Yingjun, et al. The primary observation of Cainozoic in Lantian, Shaanxi[J].Vertebrata Palasiatica, 1964, 8(2): 134-151.[张玉萍, 黄万波, 汤英俊, 等. 陕西蓝田新生界的初步观察[J]. 古脊椎动物与古人类, 1964, 8(2): 134-151.]
[28]Jia Lanpo, Zhang Yuping, Huang Wanbo, et al. Neogene of Lantian, Shaanxi Province[M]. Beijing: Science Press, 1966.[贾兰坡, 张玉萍, 黄万波, 等. 陕西蓝田新生界现场会议论文集[M]. 北京: 科学出版社, 1966.]
[29]Zhang Yuping, Huang Wanbo, Tang Yingjun, et al. Cainozoic of the Lantian Area, Shaanxi[M]. Beijing: Science Press, 1978.[张玉萍, 黄万波, 汤英俊, 等. 陕西蓝田地区新生界[M]. 北京: 科学出版社, 1978.]
[30]Liu Dongsheng. Loess and the Environment[M]. Beijing: China Ocean Press, 1985.[刘东生. 黄土与环境[M]. 北京: 科学出版社, 1985.]
[31]An Z, Kukla G, Porter S, et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130 000 years[J]. Quaternary Research, 1991, 36: 29-36.
[32]Ding Z, Rutter N, Han J, et al. A coupled environmental system formed at about 2.5 Ma in East Asia[J]. Paleogeography, Palaeoclimotology, Palaeoecology, 1992, 94: 223-242.
[33]Guo Z, Ruddiman W, Hao Q, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J]. Nature, 2002, 416: 159-163.
[34]Jiang Fuchu, Fu Jianli, Wang Shubing, et al. The age of the Yellow River passing through the Sanmen Gorge[J]. Journal of Geomechanics, 2005, 11(4): 293-301.[蒋复初, 傅建利, 王书兵, 等. 关于黄河贯通三门峡的时代[J]. 地质力学学报, 2005, 11(4): 293-301.]
[35]Wu Xihao, Jiang Fuchu, Wang Sumin, et al. The age of the Yellow River passing through the Sanmenxia Gorge to the eastern China Sea[J]. Quaternary Sciences, 1998, (2): 188.[吴锡浩, 蒋复初, 王苏民, 等. 关于黄河贯通三门峡东流入海问题[J]. 第四纪研究, 1998, (2): 188.]
[36]Zhang Chaofeng. Evolution and Dynamics Mechanism of Weihe Graben[D]. Xi’an: Northwest University, 2011.[张朝锋. 渭河地堑的形成演化及其动力学机制[D]. 西安: 西北大学, 2011.]
[37]The Research Group on “Active Fault System around Ordos Massif”, State Seismological Bureau. Active Fault System Around Ordos Massif[M]. Beijing: Seismology Press, 1988.[国家地震局鄂尔多斯活动断裂系课题组.鄂尔多斯周缘活动断裂系[M]. 北京: 地震出版社, 1988.]
[38]Xu Yujian, Shentu Bingming, Wang Yipeng. A preliminary study of the characteristics of the activity of the northern boundary fault belt of Weihe Basin[J]. Seismology and Geology, 1988, 10(4): 77-88.[徐煜坚, 申屠炳明, 汪一鹏. 渭河盆地北缘断裂带活动特征的初步研究[J]. 地震地质, 1988, 10(4): 77-88.]
[39]Feng Xijie, Li Xiaoni, Ren Jun, et al. Manifestations of Weihe fault at deep, middle, shallow and near-surface depth[J]. Seismology and Geology, 2008, 30(1): 264-272.[冯希杰, 李晓妮, 任隽, 等. 渭河断裂深、中、浅和近地表显示[J]. 地震地质, 2008, 30(1): 264-272.]
[40]Li Chuankui, Wu Wenyu, Qiu Zhuding. Chinese Neogene: Subdivision and correlation[J]. Vertebrata PalAsiatica, 1984, 22(3): 163-172.[李传夔, 吴文裕, 邱铸鼎. 中国陆相新第三系的初步与对比[J]. 古脊椎动物学报, 1984, 22(3): 163-172.]
[41]Xia Yong. The Sedimentary Characteristic of Cenozoic in Weihe Basin and Its Relationship with Tectonics[D]. Xi’an: Chang’an University, 2007.[夏勇.渭河盆地新生代沉积特征及与构造的关系[D]. 西安:长安大学, 2007.]
[42]National Commission on Stratigraphy. Introduction Book on China Regional Chronostratigraphic (Geo-chronologic) Scale[M]. Beijing: Geological Publishing House, 2002.[全国地层委员会. 中国区域年代地层(地质年代)表说明书[M].北京: 地质出版社, 2002.]
[43]Liu Hujun, Xue Xiangxu. Discussion on the cenozoic and its chronology in the Weihe River Basin[J]. Journal of Earth Sciences and Environment, 2004, 26(4): 1-5.[刘护军, 薛祥煦. 对渭河盆地新生界年代的讨论[J]. 地球科学与环境学报, 2004, 26(4): 1-5.]
[44]Liu Hujun. Formation and Evolution of the Weihe River Basin and Uplift of the Eastern Qinling Mountains[D]. Xi’an: Northwest University, 2004.[刘护军. 渭河盆地的形成演化与东秦岭的隆升[D]. 西安: 西北大学, 2004.]
[45]Sun Xiuyu, Fan Yongxiu, Deng Cilan. Cenozoic sporo-pollen assemblage of the Weihe Basin, Shaanxi[J]. Bulletin of the Chinese Academy of Geological Sciences—Journal of Institute of Geology, 1980, 1(1): 84-113.[孙秀玉, 范永琇, 邓茨兰. 渭河盆地新生代孢粉组合[J]. 中国地质科学院院报地质研究所分刊, 1980, 1(1): 84-113.]
[46]Deng Tao. Evolution of the Late Cenozoic mammalian faunas in the Linxia Basin and its background relevant to the uplift of the Qinghai-Xizang Plateau[J]. Quaternary Sciences, 2004, 24(4): 413-420.[邓涛. 临夏盆地晚新生代哺乳动物群演替与青藏高原隆升背景[J]. 第四纪研究, 2004, 24(4): 413-420.]
[47]Li Yuqing, Wu Wenyu. Miocene Artiodactyla of Lingtung and Lantian, Shensi[C]∥Professional Papers of Stratigraphy and Paleontology.Beijing: Geological Publishing House, 1978, 7: 127-135.[李玉清, 吴文裕. 陕西临潼蓝田中新世偶蹄类化石[C]∥地质古生物论文集(第七辑).北京:地质出版社, 1978, 7: 127-135.]
[48]Zhang Yunxiang, Xue Xiangxu. Discusses on subdivision of late Miocene in Lantian area, middle of Shaanxi[J]. Northwest Geoscience, 1996, 17(1): 59-62.[张云翔, 薛祥煦. 陕西蓝田地区新第三纪地层划分的几点讨论[J]. 西北地质科学, 1996, 17(1): 59-62.]
[49]Li J, Zhang J, Song C, et al. Miocene Bahean stratigraphy in the Longzhong Basin, northern central China and its implications in environmental change[J]. Science in China (Series D), 2006, 49(12): 1 270-1 279.
[50]Kaakinen A, Lunkka J. Sedimentation of the Late Miocene Bahe Formation and its implications for stable environments adjacent to Qinling Mountains in Shaanxi, China[J]. Journal of Asian Earth Sciences, 2003, 22: 67-78.
[51]Kaakinen A. A Long Terrestrial Sequence in Lantian—A Window into the Late Neogene Palaeoenvironments of Northern China[D]. Helsinki: University of Helsinki, 2005.
[52]An Zhisheng, Sun Donghuai, Chen Mingyang, et al. Red clay sequences in Chinese Loess Plateau and recorded paleoclimate events of the late Tertiary[J]. Quaternary Sciences, 2000, 20(5): 435-446.[安芷生, 孙东怀, 陈明扬, 等.黄土高原红粘土序列与晚第三纪的气候事件[J]. 第四纪研究, 2000, 20(5): 435-446.]
[53]Chinese Association for Quaternary Research. Proceedings of the Symposium on Quaternary Geology in the Sanmenxia Gorge[C]. Beijing: Science Press, 1959.[中国第四纪研究委员会. 三门峡第四纪地质会议文集[C]. 北京:科学出版社, 1959.]
[54]Yuan Fengdian. Discussions on the Cenozoic and the lower Quaternary boundary in Weihe River Regions[J]. Communication of General Petrolic Investigations in Shan Gan Ning Regions, 1976, 2: 22-32.[袁凤钿.渭河地区新生界及第四系下界的讨论[J]. 陕甘宁石油普查通讯, 1976, 2: 22-32.]
[55]Sun Jianzhong. On “Yellow Sanmen” and “Green Sanmen”[J]. Journal of Xi’an College of Geology, 1986, 8(4): 42-45.[孙建中. 关于“黄三门”与“绿三门”[J]. 西安地质学院学报, 1986, 8(4): 42-45.]
[56]Sun Jianzhong, Zhao Jingbo, Wei Mingjian, et al. New palaeomagnetic data of Wujiabu section[J]. Hydrogeology and Engineering Geology, 1988, 5: 44-48.[孙建中, 赵景波, 魏明建, 等. 武家堡剖面古地磁新资料[J]. 水文地质工程地质, 1988, 5: 44-48.]
[57]Yan Yongding. The environmental changes, exploitation and utilization of the Luyang Lake Basin[J]. Geology of Shaanxi, 1988, 6(1): 65-75.[阎永定. 卤阳湖区的环境变迁及其开发利用[J]. 陕西地质, 1988, 6(1): 65-75.]
[58]Ge Tongming, Fan Limin, Xu Xing, et al. Magnetostratigraphic study for borehole W7 from Yancun, Weinan[J]. Marine Geology & Quaternary Geology, 1991, 11(4): 59-71.[葛同明, 樊利民, 徐行, 等. 渭南阎村W7孔岩心样品的古地磁学研究[J]. 海洋地质与第四纪地质, 1991, 11(4): 59-71.]
[59]Hu Wei, Yue Leping, Tian Xinhong. On the magnetostratigraphy of the Songjia-Beigou section, Youhe, Weinan[J]. Geology of Shaanxi, 1993, 11(2): 26-32.[胡巍, 岳乐平, 田新红. 渭南沋河宋家北沟剖面磁性地层学研究[J]. 陕西地质, 1993, 11(2): 26-32.]
[60]Wang Shubing, Jiang Fuchu, Wu Xihao, et al. The connotation and significance of Sanmen Formation[J]. Quaternary Sciences, 2004, 45(1): 116-123.[王书兵, 蒋复初, 吴锡浩, 等. 三门组的内涵及其意义[J]. 第四纪研究, 2004, 45(1): 116-123.]
[61]Zheng H, An Z, Shaw J. New contribution to Chinese Plio-Pleistocene magnetostratigraphy[J]. Physics of the Earth and Planetary Interiors, 1992, 70: 146-153.
[62]Liu J, Zhang P, Lease R, 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, 2012, 584(22): 281-296.
[63]Liu Chiyang, Zhao Hongge, Gui Xiaojun, et al. Space-time coordinate of the evolution and reformation and mineralization response in Ordos Basin[J]. Acta Geologica Sinica, 2006, 12(3): 113-124.[刘池洋, 赵红格, 桂小军, 等. 鄂尔多斯盆地演化—改造的时空坐标及其成藏(矿)响应[J]. 地质学报, 2006, 12(3): 113-124.]
[64]Zhang Y, Mercier J, Vergely P. Extension in the graben systems around the Ordos(China), and its contribution to the extrusion tectonics of south China with respect to Gobi-Mongolia[J]. Tectonophysics, 1998, 285: 41-75.
[65]Zhang Y, Ma Y, Yang N, et al. Cenozoic extensional stress evolution in North China[J]. Journal of Geodynamics, 2003, 36: 591-613.
[66]Yuan Baoyin, Tang Guoan, Zhou Liping, et al. Control action on the geomorphic differentiation in Loess Plateau and the formation of Yellow River by Cenozoic tectogenesis[J]. Quaternary Sciences, 2012, 32(5): 829-838.[袁宝印, 汤国安, 周力平, 等. 新生代构造运动对黄土高原地貌分异与黄河形成的控制作用[J]. 第四纪研究, 2012, 32(5): 829-838.]
[67]Liu Suowang, Gan Jiasi. The system of Fenwei rift[J]. Crustal Deformation and Earthquake, 1981, (3): 110-123.[刘锁旺, 甘家思. 汾渭裂谷系[J]. 地壳形变与地震, 1981, (3):110-123.]
[68]Zhu Zhaoyu. The formation of river terraces and evolution of drainage system in the middle Yellow River[J]. Acta Geographica Sinica, 1989, 44(4): 429-440.[朱照宇. 黄河中游河流阶地的形成与水系演化[J]. 地理学报, 1989, 44(4): 429-440.]
[69]Lin A, Yang Z, Sun Z, et al. How and when did the Yellow River develop its square bend?[J]. Geology, 2001, 29(10): 951-954.
[70]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 throuth Sanmen Gorges[J]. Chinese Science Bulletin, 2005, 50(7): 657-664.
[71]Xing Zuoyun, Zhao Bin, Tu Meiyi, et al. The formation of the Fenwei rift valley[J]. Earth Science Frontiers, 2005, 12(2): 247-262.[邢作云, 赵斌, 涂美义, 等. 汾渭裂谷系与造山带耦合关系及其形成机制研究[J]. 地学前缘, 2005, 12(2): 247-262.]
[72]Zhang G, Meng Q, Yu Z, et al. Orogensis and dynamics of the Qinling Orogen[J]. Science in China (Series D), 1996, 39(3): 225-234.
[73]Zhang Guowei, Zhang Benren, Yuan Xuecheng, et al. Qinling Orogenic Belt and Continental Dynamics[M]. Beijing: Science Press, 2001.[张国伟, 张本仁, 袁学诚, 等. 秦岭造山带与大陆动力学[M]. 北京: 科学出版社, 2001.]
[74]Dong Y, Zhang G, Neubauer F, et al. Tectonic evolution of the Qinling orogen, China: Review and synthesis[J]. Journal of Asian Earth Sciences, 2011, 41: 213-237.[ZK)][FL)]
[1] 潘留杰, 张宏芳. NEX-BCC模式对秦岭及周边地区气候变化的模拟及预估[J]. 地球科学进展, 2018, 33(9): 933-944.
[2] 王斌, 常宏, 段克勤. 秦岭新生代构造隆升与环境效应:进展与问题[J]. 地球科学进展, 2017, 32(7): 707-715.
[3] 陈鹏, 施炜. 南秦岭造山带韧性剪切系中—晚侏罗世运动学分析与力学机制探讨[J]. 地球科学进展, 2015, 30(1): 69-77.
阅读次数
全文


摘要