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浙江省栖霞组沉积微相、韵律、沉积旋回及层序地层学分析

何海清

何海清. 浙江省栖霞组沉积微相、韵律、沉积旋回及层序地层学分析[J]. 石油实验地质, 1997, 19(2): 127-132. doi: 10.11781/sysydz199702127
引用本文: 何海清. 浙江省栖霞组沉积微相、韵律、沉积旋回及层序地层学分析[J]. 石油实验地质, 1997, 19(2): 127-132. doi: 10.11781/sysydz199702127
He Haiqing. DEPOSITIONAL MICROFACTES, RHYTHMS, CYCLES AND SEQUENCE STRATIGRAPHY OF QIXIA FORMATION IN ZHEJIANG PROVINCE, CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1997, 19(2): 127-132. doi: 10.11781/sysydz199702127
Citation: He Haiqing. DEPOSITIONAL MICROFACTES, RHYTHMS, CYCLES AND SEQUENCE STRATIGRAPHY OF QIXIA FORMATION IN ZHEJIANG PROVINCE, CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1997, 19(2): 127-132. doi: 10.11781/sysydz199702127

浙江省栖霞组沉积微相、韵律、沉积旋回及层序地层学分析

doi: 10.11781/sysydz199702127
详细信息
    作者简介:

    何海清 男 30岁 工程师 沉积、大地构造和石油地质

DEPOSITIONAL MICROFACTES, RHYTHMS, CYCLES AND SEQUENCE STRATIGRAPHY OF QIXIA FORMATION IN ZHEJIANG PROVINCE, CHINA

  • 摘要: 本文以沉积微相及生物生态分析为基础,对研究区3条剖面栖霞组的沉积韵律、沉积旋回、沉积环境进行了研究,并在此基础上分析了层序界面、沉积层序及各沉积体系域的沉积特征。认为研究区栖霞组总体形成于潮下低能开阔无障壁的碳酸盐级坡沉积背景,其中可识别出两类界面,4个沉积层序,根据界面特征及准层序叠加型式划分出海度体系域(TST)和高水位体系域(HST)。

     

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    [2] Galloway W E.Genitic Stratigraphic Sequence in Basin Analysis I:and Genesis of Flooding-Surface Bounded Depositional Unites. AAPG.1989,73(2):125-143
    [3] Vail P R et al. Seismic Stratigraphy and Cloble Change of Sea-level. In:Payton C E. ed. Seismic Stratigraphy-Application to Hydrocarbon Exploration. AAPG Memoir 1977.26:51-97
    [4] Van Wagoner J C et al. An Overview of the Fundamentals of Sequence Stratigraphy and Key Definitions. In; Wilgus C K et al eds. Sea-level Changes: an Integrated Approach. Society of Economic Paleontologists and mineralogists Special Publication 1988,42:125-154
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    [6] 薛良清.层序地层学研究现状、方法与前景.石油勘探与开发,1995,22(5):8-13
    [7] 沙庆安,吴望始,傅家谟主编,黔硅地区二叠系综合研究-兼论含油气性.北京:科学出版社,1990
    [8] 陈中强.高分辨率层序地层学的研究基础-准层序的识别.地层学杂志.1995,19(1):36-46
    [9] 刘本培,李儒峰,尤德宏.黔南独山石炭系层序地层及麦蜷带冰川型全球海平面变化.地球科学-中国地质大学学报,1994,19(5):553-564
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出版历程
  • 收稿日期:  1996-04-15
  • 刊出日期:  1997-04-25

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