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锶同位素地层学在碎屑岩成岩研究中的应用

黄思静,  石和,  张萌,  沈立成,  武文慧

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文章导航 > 沉积学报  > 2002 >  20(3): 359-366
黄思静, 石和, 张萌, 沈立成, 武文慧. 锶同位素地层学在碎屑岩成岩研究中的应用[J]. 沉积学报, 2002, 20(3): 359-366.
引用本文: 黄思静, 石和, 张萌, 沈立成, 武文慧. 锶同位素地层学在碎屑岩成岩研究中的应用[J]. 沉积学报, 2002, 20(3): 359-366.
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HUANG Si-jing, SHI He, ZHANG Meng, SHEN Li-cheng, WU Wen-hui. Application of Strontium Isotope Stratigraphy to Diagenesis Research[J]. Acta Sedimentologica Sinica, 2002, 20(3): 359-366.
Citation: HUANG Si-jing, SHI He, ZHANG Meng, SHEN Li-cheng, WU Wen-hui. Application of Strontium Isotope Stratigraphy to Diagenesis Research[J]. Acta Sedimentologica Sinica, 2002, 20(3): 359-366.
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锶同位素地层学在碎屑岩成岩研究中的应用

  • 油气藏地质及开发工程国家重点实验室,成都理工大学沉积地质研究所,成都,610059

基金项目: 国家自然科学基金项目(批准号:49972044)资助
详细信息
    作者简介:

    黄思静,男,1949年出生,教授,博士生导师,沉积学

  • 中图分类号: P588.2

Application of Strontium Isotope Stratigraphy to Diagenesis Research

  • State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation,Chengdu University of Technology, Chengdu,610059

    摘要
  • 摘要: 基于同一地质历史时期海水的锶同位素组成为一定值的锶同位素地层学基本原理,可将锶同位素地层学用于碎屑岩成岩作用研究,以评价海相和非海相对成岩作用的影响.三个不同类型的研究实例说明:1)海相碎屑岩成岩流体的锶同位素组成的演化途径有较好的规律性,陆相影响随成岩作用的进行而增加,相对晚期的碳酸盐胶结物的87Sr/86Sr比值通常高于相对早期的碳酸盐胶结物,变化的本底值即为同期海水的锶同位素组成,该数值为一定值;2)有沉积期深源锶和非同期海相影响的陆相碎屑岩中,碳酸盐胶结物的锶同位素比值可能低于大陆淡水,但埋藏成岩过程中相对晚期的碳酸盐胶结物的87Sr/86Sr比值仍高于相对早期的碳酸盐胶结物;3)当深部流体影响碎屑岩的整个成岩过程时,深源锶的烙印可以抹掉或减少不同成岩阶段不同程度陆相影响造成的各种碳酸盐胶结物之间锶同位素组成的差别,使各种碳酸盐胶结物都具有很低的87Sr/86Sr比值,因而缺乏其它沉积盆地中常见的相对晚期碳酸盐胶结物87Sr/86Sr比值高于早期胶结物的一般模式。
    Abstract: Based on the fundamental principle of StrontiumIsotope Strati graphy(SIS），i.e. strontium isotope composition of seawater is a determined value during the same geological time,we can apply the SISto the research of clastic diagenesis in order to esti matethe effect of marine f acies and non- mari ne facies on diagenesis. three eXamples for t he application from Ahujiangkou Basin,Southern China Sea,ordos Basin,and Bohai wan Basi nare shown as follows ：(1)the composition of stronti umisotope of marine clastic diagenesisfluid developed in a regular pathway.Because of the dissolution of feldspar and other terri genous silicate minerals in diagenesis，the ratio of 87Sr/86Sr of later carbonate cements in diagenesis are usually higher than that of earlier one，and the ori ginal value of the evolution process is the ratio of 87Sr/86Sr of sea water in the same term，which is a determined value.(2)the ratio of 87Sr/86Sr of carbonate cement in terrestrial sandstones may be lower than that of continental meteoric water when the strontiumfromt he mantle influenced the syngenesis water,or the marine facies influenced the diagenesis water by dissolution of older terri genous carbonate rock fragments. However,the ratio of 87Sr/86Sr of carbonate cement preci pitated during later burial diagenesis is also higher than that precipitated during earlier period.(3)When the fluid fromthe mantle controlled the full diagenesis process,and if the inference from mantle strontiumis strong enough to erase or to decrease the difference of strontium isotope composition of various carbonate cements caused by the terrestrial effect in different diagenesis period or different diagenesis degrees，the ratio of87Sr/86Sr of carbonate cements precipitated in different diagenesis periods are all very low and，theref ore，it is lack of the evolution pattern,which often appears in other sedimentary basin,and the ratio of 87Sr/86Sr of carbonate cement precipitated during later burial diagenesis is higher than that precipitated during earlier period.
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  • 收稿日期:  2001-12-17
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  • 刊出日期:  2002-09-10

目录

    锶同位素地层学在碎屑岩成岩研究中的应用

    • 油气藏地质及开发工程国家重点实验室,成都理工大学沉积地质研究所,成都,610059
      • 基金项目:  国家自然科学基金项目(批准号:49972044)资助
      作者简介:

      黄思静,男,1949年出生,教授,博士生导师,沉积学

    • 收稿日期: 2001-12-17
    • 修回日期: 2002-05-17
    • 刊出日期: 2002-09-10

    • 中图分类号: P588.2

    摘要: 基于同一地质历史时期海水的锶同位素组成为一定值的锶同位素地层学基本原理,可将锶同位素地层学用于碎屑岩成岩作用研究,以评价海相和非海相对成岩作用的影响.三个不同类型的研究实例说明:1)海相碎屑岩成岩流体的锶同位素组成的演化途径有较好的规律性,陆相影响随成岩作用的进行而增加,相对晚期的碳酸盐胶结物的87Sr/86Sr比值通常高于相对早期的碳酸盐胶结物,变化的本底值即为同期海水的锶同位素组成,该数值为一定值;2)有沉积期深源锶和非同期海相影响的陆相碎屑岩中,碳酸盐胶结物的锶同位素比值可能低于大陆淡水,但埋藏成岩过程中相对晚期的碳酸盐胶结物的87Sr/86Sr比值仍高于相对早期的碳酸盐胶结物;3)当深部流体影响碎屑岩的整个成岩过程时,深源锶的烙印可以抹掉或减少不同成岩阶段不同程度陆相影响造成的各种碳酸盐胶结物之间锶同位素组成的差别,使各种碳酸盐胶结物都具有很低的87Sr/86Sr比值,因而缺乏其它沉积盆地中常见的相对晚期碳酸盐胶结物87Sr/86Sr比值高于早期胶结物的一般模式。

    English Abstract

    黄思静, 石和, 张萌, 沈立成, 武文慧. 锶同位素地层学在碎屑岩成岩研究中的应用[J]. 沉积学报, 2002, 20(3): 359-366.
    引用本文: 黄思静, 石和, 张萌, 沈立成, 武文慧. 锶同位素地层学在碎屑岩成岩研究中的应用[J]. 沉积学报, 2002, 20(3): 359-366.
    shu
    HUANG Si-jing, SHI He, ZHANG Meng, SHEN Li-cheng, WU Wen-hui. Application of Strontium Isotope Stratigraphy to Diagenesis Research[J]. Acta Sedimentologica Sinica, 2002, 20(3): 359-366.
    Citation: HUANG Si-jing, SHI He, ZHANG Meng, SHEN Li-cheng, WU Wen-hui. Application of Strontium Isotope Stratigraphy to Diagenesis Research[J]. Acta Sedimentologica Sinica, 2002, 20(3): 359-366.
    shu

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