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首页|期刊导航|沉积与特提斯地质|柴西开特米里克地区干柴沟组米氏旋回及湖平面变化特征

柴西开特米里克地区干柴沟组米氏旋回及湖平面变化特征

徐为鹏 伊海生 唐闻强 陈云 陈晓冬 邢浩婷 宋伟 崔荣龙 乔富海

沉积与特提斯地质2023,Vol.43Issue(4):712-721,10.
沉积与特提斯地质2023,Vol.43Issue(4):712-721,10.DOI:10.19826/j.cnki.1009-3850.2021.04005

柴西开特米里克地区干柴沟组米氏旋回及湖平面变化特征

Characteristics of the Milankovitch cycles and lake-level changes in the Ganchaigou Formation of the Kaitemirike area,western Qaidam

徐为鹏 1伊海生 1唐闻强 2陈云 1陈晓冬 3邢浩婷 3宋伟 3崔荣龙 3乔富海3

作者信息

  • 1. 成都理工大学沉积地质研究院,四川 成都 610059||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. 成都理工大学沉积地质研究院,四川 成都 610059||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||中国石油青海油田分公司,甘肃 敦煌 736202
  • 3. 中国石油青海油田分公司,甘肃 敦煌 736202
  • 折叠

摘要

Abstract

At present,the research on Milankovitch cycles in the Qaidam Basin is generally based on the discussion of the shallow-water sedimentary facies strata in the piedmont,but it remains to be explored whether the Milankovitch cycle characteristics are recorded in the deep-water facies strata.In this study,the Milankovitch sedimentary cycles of deep lacustrine strata in the Kaitemilik area in the west of the basin have been discussed through spectral analyses and filter analyses of natural gamma logging curves of the upper Ganchaigou Formation(N1)and the upper part of lower Ganchaigou Formation(E32)in Well K2.The results show that the stratigraphic cycles of the upper Ganchaigou Formation(N1)and the upper part of lower Ganchaigou Formation(E32)in this area have a good correlation with the earth's orbital cycle parameters of Milankovitch,indicating that the astronomical orbital cycle had a significant effect on the stratigraphic deposition in this area.On this basis,the Fischer plot and the sedimentary characteristics of the strata indicate that the lake level near the upper and lower boundary of Ganchaigou Formation(~38.1-32.8 Ma)experienced a relatively long period of fluctuation.The upper part of lower Ganchaigou Formation was formed in the rising stage of the lake level,which was mainly controlled by the eccentricity cycle in the Milankovitch cycle,and the climate was relatively warm and humid,corresponding to the high stage of lake level.The upper Ganchaigou Formation was deposited in the falling stage of the lake level,which was mainly controlled by the axial slope cycle in the Milankovitch cycle,and the climate was relatively cold and dry,corresponding to the low stage of lake level.

关键词

柴达木盆地/自然伽马/米氏旋回/Fischer图解/湖平面

Key words

Qaidam Basin/natural gamma/Milankovitch cycle/Fischer plot/lake level

分类

天文与地球科学

引用本文复制引用

徐为鹏,伊海生,唐闻强,陈云,陈晓冬,邢浩婷,宋伟,崔荣龙,乔富海..柴西开特米里克地区干柴沟组米氏旋回及湖平面变化特征[J].沉积与特提斯地质,2023,43(4):712-721,10.

基金项目

国家自然科学基金项目(41972115) (41972115)

中国石油科技部重大专项(2019B-0309) (2019B-0309)

沉积与特提斯地质

OA北大核心CSCDCSTPCD

1009-3850

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