地球科学进展 ›› 2009, Vol. 24 ›› Issue (2): 172 -180. doi: 10.11867/j.issn.1001-8166.2009.02.0172

研究论文 上一篇    下一篇

四川类前陆盆地须家河组震积岩的发现及其研究意义
戴朝成 1,郑荣才 1,朱如凯 2,翟文亮 1,高红灿 1   
  1. 1. 成都理工大学油气藏地质及开发工程国家重点实验室,四川 成都 610059;
    2. 中国石油勘探开发研究院油气储层重点实验室,北京 100083
  • 收稿日期:2008-10-29 修回日期:2008-12-25 出版日期:2009-02-10
  • 通讯作者: 戴朝成 E-mail:daichaocheng@qq.com
  • 基金资助:

    国家重大专项项目“大型油气田及煤层气开发”(编号:2008ZX05000-003-01)资助.

The Discovery and Significance of Seismites from Xujiahe Formation in Sichuan Analogous Foreland Basin

Dai Chaocheng 1,Zheng Rongcai 1,Zhu Rukai 2,Zhai Wenliang 1,Gao Hongcan 1   

  1. 1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology,Chengdu 610059, China;
    2.Key Laboratory of Oil and Gas Reservoir of CNPC, Beijing 100083,China
  • Received:2008-10-29 Revised:2008-12-25 Online:2009-02-10 Published:2008-02-10

四川盆地是扬子地块上的一个多旋回类前陆盆地,盆地边缘长期剧烈的构造活动控制着上三叠统须家河组的沉积作用。通过地表剖面和岩芯观察,首次在该盆地上三叠统须家河组地层中识别出微裂缝、微褶皱层、微断层、液化砂岩构造、球—枕构造和角砾岩等典型的软沉积变形构造的地质记录,这些变形构造可能与印支构造运动期的地震活动有关。越靠近断裂带附近,软变形构造呈明显增加的趋势,表明震积岩的分布与龙门山和米仓山—大巴山构造活动有关。因此,研究该盆地须家河组震积岩,对了解控制盆地边界的龙门山和米仓山—大巴山造山带的活动史具有重要意义。

    The sedimentary processes of the Upper Triassic Xujiahe Formation were controlled by the long-term tectonic activity in the peripheral zones of Sichuan basin, a mult-episodic para-foreland basin of the Yangtze block. Based on the outcrop and the core observations, a series of soft sedimentary deformation structures were recognized for the first time in the Triassic Xujiahe formation in Sichuan Basin; these structures include micro-cracks, micro-folds, micro-faults, liquefied sand structure, ball-and-pillow structures and eautochthnous breccias, and so on. These autochthonous structures are here suggested to having been formed related to seismic activity during Indosinian tectonic episode. The increase in abundance of these soft deformation structures towards the outer peripheral zone of the basin to the west and north respectively suggests a causal connection to the overthrusting of Longmenshan to the west and Micangshan-Dabashan to the north fold-thrust belts, Therefore, to a broader extent, this study is of great significance for us to understand the tectonic history of Sichuan basin and adjacent Longmenshan and Micangshan-Dabashan fold-thrust belts.

中图分类号: 

[1] Seilacher A. Fault-graded bed interpreted as seismites[J].Sedimentology,1969,13(1/2):155-159.
[2] Du Yuansheng,Han Xin. Seismo-deposition and seismites[J].Advances in Earth Science,2000,(4):389-394.[杜远生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,(4):389-394.]
[3] Seilacher A. Sedimentary structures tentatively attributed to seismic events[J]. Marine Geology,1984,55(1):1-12.
[4] Song Tianrui. A possible seismite-sunami sequence in Precambrian carbonate stratigraphy in Shisanling area,Beijing[J]. Chinese Science Bulletin,1988,38(8):609-611.[宋天锐.北京十三陵前寒武纪碳酸盐岩地层中的一套可能的地震—海啸序列[J].科学通报,1988,38(8):609-611.]
[5] Qiao Xiufu, Song Tianrui, Gao Linzhi, et al. Seismic sequence in carbonate rocks by vibrational liquefaction[J].Acta Geologica Sinica,1994,68(1):16-32.[乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):16-32.]
[6] Qiao Xiufu, Li Haibing, Gao Linzhi. Sinian-early Paleozoic seismic rhythms on the north China platform[J].Earth Science Frontiers,1997,4(3/4):155-160.[乔秀夫,李海兵,高林志.华北地台震旦纪—早古生代地震节律[J].地学前缘,1997,4(3/4):155-160.][7] Qiao Xiufu, Gao Linzhi. Earthquake events in Neoproterozoic and Early Paleozoic and its relationship with super continental Rodinia in North China[J].Chinese Science Bulletin,1999,44(16):1 753-1 758.[乔秀夫,高林志.华北中新元古代及早中生代地震灾变事件及与Rodinia的关系[J].科学通报,1999,44(16):1 753-1 758.]
[8] Qiao Xiufu, Gao Linzhi, Peng Yang, et al. Seismic event, sequence and tectonic significance in Canglangpu Stage in paleo-tanlu fault zone[J]. Science in China(Series D),2001,31(11):911-918.[乔秀夫,高林志,彭阳,等.古郯庐带沧浪铺阶地震事件、层序及构造意义[J].中国科学:D辑,2001,31(11):911-918.]
[9] Liang Dingyi, Nie Zetong, Wan Xiaoqiao, et al. On the seismite and seismodisconformity-take the w.hunan and w.yunnan regions as an example[J].Geoscience,1991,5(2):138-147.[梁定益,聂泽同,万晓樵,等.试论震积岩及震积不整合——以川西、滇西地区为例[J].现代地质,1991,5(2):138-147.]
[10] Liang Dingyi, Nie Zetong, Song Zhimin. A re-study on seismite and seismo-unconformity taking western Sichuan and western Yunnan as an example[J]. Earth Science,1994,19(6):845-850.[梁定益,聂泽同,宋志敏.再论震积岩及震积不整合——以川西、滇西地区为例[J].地球科学,1994,19(6):845-850.]
[11] Wu Xiantao, Yin Guoxun. Discovery of seismite and its significance of the Late Jura lacust rine deposit in Emei, Sichuan province[J].Acta Sedimentologica Sinica,1992,10(3):19-24.[吴贤涛,尹国勋.四川峨眉晚侏罗世湖泊沉积中震积岩的发现及其意义[J].沉积学报,1992,10(3):19-24.]
[12] Du Yuansheng, Zhang Chuanheng, Han Xin, et al. Earthquake events deposition and geologic significance of Kunyang group in Mid-Proterozoic in Dianxi[J].Science in China(Series D),2001,31(4):283-289.[杜远生,张传恒,韩欣,等.滇中中元古代昆阳群的地震事件沉积及其地质意义[J].中国科学:D辑,2001,31(4):283-289.]
[13] Jia Zhihai,Hong Tianqiu,Zheng Wenwu, et al.the characters and environments of the seismites of the Neoproterzoic Wangshan formation in north Anhui[J].Journal of Stratigraphy,2003,27(2):146-149.[贾志海,洪天求,郑文武,等.皖北新元古代望山组震积岩的基本特征及其形成环境分析[J].地层学杂志,2003,27(2):146-149.]
[14] Zhang Qin, Zhu Xiaomin, Zhang Jianjun, et al. The discovery of seismite and its significance in Lower Cretaceous in Liugouzhuang and Kulongshan region, Qingnan Sag, Jiuxi Basin[J].Acta Geologica Sinica,2003,77(2):158-162.[张琴,朱筱敏,张建军,等.酒西盆地青南凹陷柳沟庄—窟窿山地区下白垩统震积岩的发现及意义[J].地质学报,2003,77(2):158-162.]
[15] Zheng Rongcai,Wen Huaguo,Fan Mingtao, et al. Lithological characteristics of sublacustrine white smoke type exhalative rock of the Xiagou Formation in Jiuxi basin[J].Acta Petrologica Sinica,2006,22(12):3 027-3 038.[郑荣才,文华国,范铭涛,等.酒西盆地下沟组湖相白烟型喷流岩岩石学特征[J].岩石学报,2006,22(12):3 027-3 038.]
[16] Chen Shiyue, Yuan Wenfang, Yan Jihua. Discovery and significance of earthquake event deposits of Early Tertiary in the Jiyang depression[J].Earth Science,2003,38(3):413-424.[陈世悦,袁文芳,鄢继华.济阳坳陷早第三纪震积岩的发现及其意义[J].地质科学,2003,38(3):413-424.]
[17] Lü Hongbo, Zhang Yuxu, Xia Bangdong, et al. Syn-sedimentary Compression Structures in the Middle Triassic Flysch of the Nanpanjiang Basin, SW China[J].Geological Review,2003,49(5):449-456.[吕洪波,章雨旭,夏邦栋,等.南盘江盆地中三叠统复理石中的同沉积挤压构造——一类新的沉积构造的归类、命名和构造意义探讨[J].地质论评,2003,49(5):449-456.]
[18] Lü Hongbo, Zhang Yuxu, Xiao Guowang, et al. Earthquake slump blocks discovered in lower part of the Sailinhudong Group, Heinaobao, Southeast Bayan Obo, Inner Mongolia[J].Geological Review,2006,52(2):163-169.[吕洪波,章雨旭,肖国望,等.内蒙古白云鄂博南东黑脑包腮林忽洞群下部发现地震滑塌岩块[J].地质论评,2006,52(2):163-169.]
[19] Yuan Jing. The property and geological significance of seismites of Paleogene in Huimin sag, Shandong province[J].Acta Sedimentologica Sinica,2004,22(1):41-46.[袁静.山东惠民凹陷古近纪震积岩特征及其地质意义\[J\].沉积学报,2004,22(1):41-46.]
[20] Xia Qingsong,Tian Jingchun,Huang Changwu. Study on the recognition marks of seismites in Upper Triassic Yanchang Formation,Ordos basin,China[J].Journal of Chengdu University of Technology(Science & Technology Edition),2007,34(3):312-317.[夏青松,田景春,黄昌武.鄂尔多斯盆地上三叠统延长组震积岩识别标志研究[J].成都理工大学学报:自然科学版,2007,34(3):312-317.]
[21] Huang Hongwei,Du Yuansheng,Huang Zhiqiang, et al. Paleozoic seismites in the Nandan-Hechi basin, Guangxi and its tectonic significance[J].Geological Review,2007,53(5):592-599.[黄宏伟,杜远生,黄志强,等.广西丹池盆地晚古生代震积岩及其构造意义[J].地质论评,2007,53(5):592-599.]
[22] Li Yanling, Li Jiesen. The past one thousand years earthquakes record of Yunnan Fuxian lake[J].Advances in Earth Science, 2003,18(6):906-911.[李雁玲,李杰森.云南抚仙湖近千年地震事件记录[J].地球科学进展,2003,18(6):906-911.]
[23] Deng Kangling. Formation and evolution of Sichuan basin and domains for oil and gas exploration[J].Natural Gas Industry, 1992,12(5):7-12.[邓康龄.四川盆地形成演化与油气勘探领域[J].天然气工业,1992,12(5):7-12.]
[24] Guo Zhengwu, Deng Kangling, Han Yonghui, et al. The formation and the evolvement of Sichuan basin[M]. Beijing:Geological Publishing House,1996.[郭正吾,邓康龄,韩永辉,等.四川盆地形成与演化[M].北京:地质出版社,1996.]
[25] Tong Chongguang. Tectonic Evolution and Oil and Gas Gather of Sichuan Basin[M]. Beijing:Geological Publishing House,1985.[童崇光.四川盆地构造演化与油气聚集[M].北京:地质出版社,1985.]
[26] Wu Chongjun, Xue Shuhao. Sedimentation of Chinese Petroliferous Basin[M]. Beijing:Oil Industry Publishing House,1992.[吴崇筠,薛叔浩.中国含油气盆地沉积学[M].北京:石油工业出版社,1992.]
[27] Luo Zhili,Liu Shugen.Comments on the citation of the term “foreland basin” in the petroliferous basins of central and western  China—A review on the development of Chinese petroleum tectonics[J].Geological Review,2002,48(4):398-407.[罗志立,刘树根.评述“前陆盆地”名词在中国西部含油气盆地中的应用[J].地质论评,2002,48(4):398-407.]
[28] Zheng Rongcai,Zhu Rongkai,Zhai Wenliang,et al.Tectonic evolution and sequence filling patterns in the western Sichuan foreland-like basin in the Upper Triassic Xujiahean period[J]. Geology in China,2008,35(2):246-255.[郑荣才,朱如凯,翟文亮,等.川西类前陆盆地晚三叠世须家河期构造演化及层序充填样式[J].中国地质,2008,35(2):246-255.]
[29] Liu Hefu, Wang Zecheng, Xiong Baoxian, et al.Coupling analysis of Mesozoic-Cenozoic foreland basin and mountain system in central and western China[J]. Earth Science Frontiers, 2000,7(3):55-72.[刘和甫,汪泽成,熊保贤,等.中国中西部新生代前陆盆地与挤压造山带耦合分析[J].地学前缘,2000,7(3):55-72.]
[30] Liu Shugen, Luo Zhili, Zhao Xikui, et al. Coupling relationships of Sedimentary basin-Orogenic Belt systems and their dynamic models in west China—A case study of the Longmenshan Orogenic Belt-West Sichuan foreland basin system[J].Acta Geological Sinica,2003,77(2):177-186.[刘树根,罗志立,赵锡奎,等.中国西部盆山系统的耦合关系及其动力学模式——以龙门山造山带—川西前陆盆地系统为例[J].地质学报,2003,77(2):177-186.]
[31] Li Yong, Allen P A, Zhou Rongjun, et al. Mesozoic-Cenozoic Dynamics of Longmenshan foreland basin along the eastern Margin of the Tibetan plateau and its coupled relationship with Continnent Collision[J].Acta Geological Sinica,2006,80(8):1 101-1109.[李勇,Allen P A,周荣军,等.青藏高原东缘中新生代龙门山前陆盆地动力学及其与大陆碰撞作用的耦合关系[J].地质学报,2006,80(8):1 101-1 109.]
[32] Zheng Rongcai,Zhu Rukai,Dai Chaocheng,et al.Depositional sequence feature of the coupling process between basin and mountain of Xujiahe formation,Upper Triassic in northeastern Sichuan foreland basin[J].Acta Geological Sinica,2008,82(8):1 077-1 087.[郑荣才,朱如凯,戴朝成,等.川东北类前陆盆地须家河组盆—山耦合过程的沉积—层序特征[J].地质学报,2008,82(8):1077-1087.]
[33] Luo Zhili,Song Hongbiao,Zhao Xikui.C-subduction and its roles in the evolution of the orogenic belts in central-western china[J].Petroleum Exploration and Development,1995,22(2):1-7.[罗志立,宋鸿彪,赵锡奎.C-俯冲带及对中国中西部造山带形成的作用[J].石油勘探与开发,1995,22(2):1-7]
[34] Chen Fajing, Wang Xinwen, Zhang Guangya,et al. Tectonic features and geodynamics of mesozoic and Cenozoic foreland basins in China[J].Earth Science—Journal of China University of Geosciences,1996,21(4):366-372.[陈发景,汪新文,张光亚,等.中国中、新生代前陆盆地的构造特征和地球动力学[J].地球科学——中国地质大学学报,1996,21(4):366-372.]
[35] Zhang Jian,Li Guohui,Xie Jirong, et al. Stratigraphic division and correlation of Upper Triassic in Sichuan basin[J].Natural Gas Industry, 2006,26(1):12-15.[张健,李国辉,谢继容,等.四川盆地上三叠统划分对比研究[J].天然气工业,2006,26(1):12-15.]
[36] Wei Chuigao,Zhang Shiqi,Jiang Zaixing, et al. Discovery and significance of seismite of silurian in Member Ⅲ at Shahejie Formation in Xianhe area of Dongying sag[J]. Acta Sedimentologica Sinica, 2006,24(6):798-805.[魏垂高,张世奇,姜在兴,等.东营凹陷现河地区沙三段震积岩特征及其意义[J].沉积学报,2006,24(6):798-805.]
[37] Zhu Haizhi. Liquefaction of sandy soil during earthquakes and structural index of liquefaction[J].Chinese Science Bulletin, 1971,24:1 127-1 131.[朱海之.砂土震动液化与液化结构指数[J].科学通报,1971,24:1 127-1 131.]
[38] Smith B. Ball-or-pillow-form structure in sandstone[J].Marine Geology,1916,3:146-156.
[39] Qiao Xiufu, Li Haibing. Pillow, Ball-and-pillow structures: Paleo-seismic records within strata[J].Geological Review,2008,54(6):721-730.[乔秀夫,李海兵.枕、球—枕构造:地层中的古地震记录[J].地质论评,2008,54(6):721-730.]
[40] Spallctta C, Vai G B. Upper Devonian intraclast parabreccias interpreted as seismites[J].Marine Geology,1984,55(1/2):133-144.
[41] Hou Fanghao,Jiang Yuqiang,Fang Shaoxian, et al. Sedimentary model of sandstone in second and fourth members of Xiangxi formation in the Upper Triassic of Sichuan basin[J].Acta Petrolei Sinica,2005,26(2):30-37.[侯方浩,蒋裕强,方少仙,等.四川盆地上三叠统香溪组二段和四段砂岩沉积模式[J].石油学报,2005,26(2):30-37.]
[42] Wang Huaai,Zhong Jianhua,Chen Xin, et al. Characteristics of Cretaceous Seismite in the Tamuchage Depression, Mongolia, and Its Significance[J].Acta Geological Sinica,2008,82(8):1 088-1 093.[王化爱,钟建华,陈鑫,等.蒙古塔木察格坳陷白垩系震积岩特征及其地质意义[J].地质学报,2008,82(8):1 088-1 093.]
[43] Li Dewei.Mechanism and prediction of the intraplate earthquakes:An example from Wenchuan earthquake in Sichuan province[J].Geological Science and Technology Information,2008,27(5):1-6.[李德威.大陆板内地震的发震机理与地震预报[J].地质科技情报, 2008,27(5):1-6.]
[44] Wang Jinqi.Recognition on the main episode of Indo-China movement in the Longmen mountains—A rereview on the Anxian tectonic movement[J].Acta Geologica Sichuan,2003,23(2):65-69.[王金琪.龙门山印支运动主幕辨析——再论安县构造运动[J].四川地质学报,2003,23(2):65-69.]
[45] Liu Shugen,Zhao Xikui,Luo Zhili, et al. Study on the tectonic events in the system of the Longmen mountain-west Sichuan foreland basin, China[J].Journal of Chengdu University of Technology,2001,28(3):221-230.[刘树根,赵锡奎,罗志立,等.龙门山造山带——川西前陆盆地系统构造事件研究[J].成都理工学院学报,2001,28(3):221-230.]

[1] 杜远生,韩 欣. 论震积作用和震积岩[J]. 地球科学进展, 2000, 15(4): 389-394.
阅读次数
全文


摘要