全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
地质学报  2002 

东昆仑早―中二叠世生物礁建造特征

, PP. 145-154

Keywords: 生物礁,早―中二叠世,控制因素,造礁作用,东昆仑

Full-Text   Cite this paper   Add to My Lib

Abstract:

本文从造礁群落演替、层序地层和海平面升降等方面,结合大地构造引起基底沉降的证据,论述了东昆仑早―中二叠世生物礁的建造特征。东昆仑生物礁中包含6种造礁群落,各群落生物组成和结构与环境因素密切相关,4个生物礁发育阶段中群落演替关系显著。礁相地层中可识别SB_1层序界面1个和SB_2界面4个,可划分出5个三级层序。层序的沉积相序显示清晰,按曲线形态将海平面升降归为4个周期。据区域地层和相分布资料反映的古地理环境变迁,推论出石炭纪至早―中二叠世造礁期柴达木地块与羌塘地块间聚合离散的4个构造期。东昆仑生物礁的生长发育与造礁群落的演化阶段、海平面升降周期和大地构造期彼此吻合,证明生物礁建造与各控制因素间具密切制约关系。海西中―晚期柴达木地块与羌塘地块的开―合转换,为生物大规模造礁创造了长期稳定的环境。

References

[1]  陈学时,耿忠霞.1999.广西十万大山盆地下二叠统生物礁古油藏及隐伏礁预测.地质学报,73(4):350~359).
[2]  范嘉松.1988.古代生物礁研究中的若干问题,兼论我国西南地区二叠系生物礁的类型.石油与天然气地质,9(1):46~55.
[3]  洪天求,黄明,G.弗莱斯.2000.中国西南地区泥盆纪的生物礁.地质学报(英文版),74(4):727~739.
[4]  姜春发,杨经绥,冯秉贵,朱至直,赵民,柴耀楚.1992.昆仑开合构造.北京:地质出版社.
[5]  沈远超,杨金中,刘铁兵,李光明,曾庆栋.2000.新疆东昆仑祁漫塔格地区发现蛇绿岩.地质论评,46(1):90.
[6]  王永标,张克信,龚一鸣,张志,骆满生.1998.东昆仑地区早二叠世生物礁带的发现及其重要意义.科学通报,43(6):630~632.
[7]  吴亚生.1989.广西隆林下二叠统生物礁的综合研究.地质论评,35(1):52~59.
[8]  吴亚生,范嘉松.2001.根据生物礁定量计算茅口期全球海平面变化幅度.中国科学D,31(3):233~242.
[9]  曾允孚,王正瑛,田洪均.1983广西大厂龙头山泥盆纪生物礁的研究.地质论评,29(4):321~330.
[10]  Barnes R S K, Hughes R N. 1982, An introduction to marine ecology. Oxford London: Blackwell Scientific Publications,
[11]  Fan J. 1988. Some problems in the study of ancient reefs - Discussion of the type of the Permian reefs in Southwest China. Oil and Gas Geology, 9(1): 46~55 (in Chinese).
[12]  Fluegel E. 1982. Microfacies analysis of limestone. New York:Springer-Verlag.
[13]  Fluegel E. et al. 1992. Phanerozoic reefevolution: basic questions and date base. Facies, 26: 167~278.
[14]  Gong Enpu and Guan Guangyue. 1998. Evolution of the Carboniferous Reef Communities in China. Geological Review, 44(2): 164~.
[15]  Heckel P H. 1974. Carbonate buildups in the geologic record: a review. In: Laporte L F. ed. Reefs in time and space. Soc. Econ.Paleontologists Mineralogists Spec. Pub., 18: 90~ 154.
[16]  Hong Tianqiu, Huang Ming, Flajs G. A study of Devonian reefs from southern China. Acta Geologica Sinica (English Editon), 74 (4):727~739.
[17]  Jiang Yuehua,Yue Wenzhe,Liu Zuhan,Yang Mengda,Jin Shanyu,Wu Jinyun. 2000. An application of carbon and oxygen isotopes to Late Permian feef diagenesis in Hunan Province. Geological Review, 46(2): 196~.
[18]  Jiang C, Yang J, Feng B, Zhu Z, Zhao M, Chai Y. 1992. Opening closing tectonics of Kunlun Mountains. Geol. Pub. House, Beijing, Geol. Memoirs , 5 (12) (in Chinese).
[19]  Longman M W. 1981. A process approach to recognizing facies of reef complexes. In: Toomey D F. ed. European fossil reef models.Soc. Econ. Paleontologists Mineralogists Spec. Pub., 30: 9~40.
[20]  Shen Yuanchao, Yang Jinzhong, Liu Tiebing, Li Guangming, Zeng Qingdong. 2000. Ophiolite found in the Qimantag area, East Kunlun Mountains, Xinjiang. Geological Review, 46( 1 ): 90.
[21]  Tian S, Cui J. Xu Z. 1997. Discovery of a huge Early Permian reef zone and its significance in the Tethyan evolution. Continental Dynamics, 2 (1): 70~72.
[22]  Troell A R. 1962. Lower Mississippian bioherms of southwestern Missouri and northwestern Arkansas. J. Sed. Petrology, 32: 629~664.
[23]  Wang Y, Zhang K, Gong Y, Zhang Z, Luo M. 1998. Discovery and its significance of Early Permian reefs in the East Kunlun area.Chinese Science Bulletin, 43 (6): 630~632 (in Chinese).
[24]  Wang Yongbiao, Xu Guirong, Lin Qixiang, Gong Shuyun. 2000.Distribution of rare earth elements in Early Permian reef-island ocean sediments in eastern Kunlun, Acta Geologica Sinica(English Editon), 74(1): 74~83.
[25]  Wu Yasheng. 1989. The Early Permian organic reefs, Longlin county, Guangxi province. Geological Review, 35(1): 52~59.
[26]  Zeng Yunfu, Wangzhengying, Tian Hongjun. The study of the Devonian Longtoushan organic reef in Dachang, Guangxi. Geological Review, 29(4): 321~330.
[27]  曹永清,罗照华,邓晋福,赵国春,荆旭华.1999.东昆仑柴达木北缘地区早古生代火山活动与构造演化.地质论评,1999,45(增刊):1002~1009.
[28]  范嘉松,张维.1985.生物礁的基本概念、分类及识别特征.岩石学报,1(3):45~59.
[29]  巩恩普.1993.湖南新邵巨口铺中泥盆统中泥盆世生物礁生长动力学研究.地质学报,67(3):276~286.
[30]  巩恩普,关广岳.1998.中国石炭纪生物礁造礁群落演化.地质论评,44(2):160~164.
[31]  姜月华,岳文浙,柳祖汉,杨孟达,金善鹬,武金云.2000.湖南晚二叠世生物礁成岩作用的碳、氧同位素研究.地质论评,46(2):190~196.
[32]  雷卞军,强子同,文应初.1994.川东及邻区上二叠统生物礁的白云岩化.地质论评,40(6):534~543.
[33]  田树刚,王增吉.2001.东昆仑早-中二叠世生物礁相地层层序.地球学报,22(3),243~248.
[34]  王永标,徐桂荣,林启祥,龚淑云.2000.东昆仑早二叠世礁岛海洋沉积物中稀土元素的分布.地质学报(英文版),74(1):68-73.
[35]  许志琴,李海兵,杨经绥,陈文.2001.东昆仑山南缘大型转换挤压构造带和斜向俯冲作用.地质学报,75(2):156~164.
[36]  Cao Yongqing, Luo Zhaohua, Deng Jinfu, Zhao Guochun and Jin Xuhua. 1999. Paleozoic volcanic activities and tectonic evolution of the East Kunlun Mountains the north margin of the Qaidam Basin. Geological Review, 45(supp. ): 1009~.
[37]  Chen Xueshi and Geng Zhongxia. 1999. Reef Palaeopool and Prediction of Buried Reefs in the Lower Permian Series from Shiwandashan Basin of Guangxi Province. Acta Geologica Sinica, 73(4):350~359(in Chinese with Englsih abstract).
[38]  Fan J, Zhang W. 1985. On the basic concept and classification of organic reefs and their main identifying criteria. Acta Petrologica Sinica, 1(3): 45~59 (in Chinese).
[39]  Gong Enpu. 1993. Growth dynamics of the Middle Devonian Jukoupu bioherm, Xinshao, Hunan. Acta Geological Sinica, 67 (3): 276~286(in Chinese with English abstract).
[40]  Lei Bianjun, Qiang Zitong, Wen Yingchu. 1994. Dolomitization of the Upper Permian organic reefs in eastern Sichuan and its adjacent area. Geological Review, 40(6): 534~543.
[41]  Pray L C. 1969. Micrite and carbonate cement: genetic factors in Mis sissippian bioherms (Abstract). J. Paleontology, 43: 895.
[42]  Tian S, Fan J. 2001. Early-Middle Permian reef frameworks and reef-building models in the eastern Kunlun Mountains. Acta Geologica Sinica, 75 (2): 115~125.
[43]  Wu Y, Fan J. 2001. Calculation of Maokouan eustatic ranges based on reefs. Science in China (D), 31(3): 233~242.
[44]  Xu Zhiqin, Li Haibing, Yang Jingsui, Chen Wen. 2001. A large transtression zone at the south margin of the east Kunlun Mountains and Oblique subduction. Acta Geological Sinica, 75(2): 156~164 (in Chinese with English abstract).

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133