综述与评述

沉积盆地中恢复地层剥蚀量的新方法

展开
  • ①石油大学,山东 东营 257062;②石油大学,北京 昌平 102200
王毅,男,1962年8月出生,副教授,主要从事层序地层学、构造地质学与盆地分析研究。

收稿日期: 1999-07-26

  网络出版日期: 1999-10-01

PROGRESS OF THE METHODS ON THE RECOVERY OF THE THICKNESS OF ERODED STRATA IN BASIN

Expand
  • ①University of Petroleum,Dongying,Shandong 257062,China;②University of Petroleum,Beijing 102200,China

Received date: 1999-07-26

  Online published: 1999-10-01

摘要

主要介绍了磷灰石裂变径迹分析法、沉积波动过程分析法和宇宙成因核素分析法等3种恢复和计算地层剥蚀量的新方法。它们的优点是不但给出一个剥蚀面造成的地层总的剥蚀量,还能详细刻画整个剥蚀过程,从而能计算出每一期构造抬升引起的地层剥蚀量。

本文引用格式

王 毅,金之钧 . 沉积盆地中恢复地层剥蚀量的新方法[J]. 地球科学进展, 1999 , 14(5) : 475 -481 . DOI: 10.11867/j.issn.1001-8166.1999.05.0475

Abstract

 The Apatite fission track analysis, the deposition-erosion process analysis and the cosmogenic nuclide analysis are introduced as the three new advancing methods on the recovery of the thickness of eroded strata in basin in this paper. The three new methods have the common advantage, that is: not only the general thickness of eroded strata can be obtained, but also the whole erosion process be obtained. So the thickness of eroded strata occurring in every tectonic elevated erosion period can be easily recovered by means of the new methods.

参考文献

〔1〕马文璞.区域构造解析〔M〕.北京:地质出版社, 1992. 28~37.
〔2〕真柄钦次著.石油圈闭的地质模型〔M〕.童晓光,贾承造译.武汉:中国地质大学出版社, 1991. 83~98.
〔3〕Dow W G. Kerogen studies and geological interpretation〔J〕.Journal of Geochemical Exploration, 1977, 7(2): 79~99.
〔4〕庞雄奇,陈章明,陈发景.含油气盆地地史、热史、生留排烃史数值模拟研究与烃源岩定量评价〔M〕.北京:地质出版社,1993. 16~21.
〔5〕Guidish T M. Basin evaluation using burial history calculations: an overview〔J〕. Bulletin of AAPG, 1985, 69(1): 92~104.
〔6〕Magara K著.压实与油气运移〔M〕.陈荷立,等译.北京:石油工业出版社,1981.
〔7〕Katz J B, Pheifer R N, Schunk D J. Interpretation of discontinues vitrinite reflectance profile〔J〕. Bulletin of AAPG, 1988, 72(8): 926~931.
〔8〕何生,王青玲.关于用镜质体反射率恢复地层剥蚀厚度的问题讨论〔J〕.地质论评, 1989, 35(2): 119~125.
〔9〕尹天放.多种信息综合计算剥蚀厚度方法〔J〕.石油勘探与开发, 1992, 19(5): 42~47.
〔10〕郝石生,贺志勇,高耀斌,等.恢复地层剥蚀厚度的最优化方法〔J〕.沉积学报, 1988, 6(4): 93~99.
〔11〕李明诚,李伟.利用平衡浓度研究天然气的扩散〔J〕.天然气工业, 1996, 16(1): 1~5.
〔12〕李伟.恢复地层剥蚀厚度方法综述〔J〕.中国海上油气,1996, 10(3): 167~172.
〔13〕周中毅,潘长春.沉积盆地古地温测定方法及其应用〔M〕.广州:广东科技出版社, 1992. 68~104.
〔14〕Lastett G M, Green P F, Duddy I R,et al. Thermal annealing of fission tracks in apatite 2: a quantitative analysis〔J〕. Chemical Geology, 1987, 65(1): 1~13.
〔15〕Rampino M R, Stothers R B. Flood basalt volcanism during the past 250 million years〔J〕. Science, 1988, 241: 663~668.
〔16〕Pal P C, Creer K M. Geomagnetic reversal spurts and episodes of extraterrestrial catastrophism〔J〕. Nature, 1986,320: 148~150.
〔17〕史晓颖. 35 Ma——地质历史上一个重要的周期〔J〕.地球科学, 1996, 21(3): 235~242.
〔18〕周瑶琪,吴智平,章大港,等.对地质节律与地球动力系统的思考〔J〕.地学前缘, 1997, 4(3~4): 85~94.
〔19〕徐钦琦.天文气象学〔J〕.地球科学进展, 1994, 9(2): 82~83.
〔20〕崔盛芹,吴珍汉.略论构造运动节律与构造运动序列〔J〕.地学前缘, 1997, 4(3~4): 223~233.
〔21〕刘国臣,金之均,李京昌.沉积盆地沉积—剥蚀过程定量研究的一种新方法〔J〕.沉积学报, 1995, 13(3): 23~32.
〔22〕Cerling T E, Craig H. Geomorphology and in situ cosmogenic isotopes〔J〕. Earth Planet Sci, 1994, 22: 273~317.
〔23〕周瑶琪,陆永潮,李思田,等.间断面缺失时间的计算问题〔J〕.地质学报, 1997, 71(1): 7~17.

 

文章导航

/