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四川盆地上震旦统灯影组风化壳古岩溶特征及模式分析

罗贝维 贾承造 魏国齐 杨威 谢武仁 许海龙

中国石油大学学报(自然科学版)Issue(3):8-19,12.
中国石油大学学报(自然科学版)Issue(3):8-19,12.DOI:10.3969/j.issn.1673-5005.2015.03.002

四川盆地上震旦统灯影组风化壳古岩溶特征及模式分析

Characteristics and models of weathering paleo-karst in Upper Sinian, Sichuan Basin

罗贝维 1贾承造 2魏国齐 3杨威 3谢武仁 3许海龙1

作者信息

  • 1. 中国石油勘探开发研究院,北京100083
  • 2. 中国石油天然气集团公司,北京100724
  • 3. 中国石油勘探开发研究院廊坊分院,河北廊坊065007
  • 折叠

摘要

Abstract

The development of ancient weathering crust karst in Sinian is the main factor of the breakthrough in Dengying Formation of Sichuan Basin. With a lot of outcrops, drilling coring, thin sections, seismic and well logging data, geochemis-try analysis, and on the basis of the comprehensive arguments about the two sets of weathering paleo-karst in Dengying For-mation, weathering paleo-karst characteristics and differences between the vertical and horizontal structures were studied to further establish corresponding weathering paleo-karst models. It is concluded that the weathering paleo-karsts in Dengying Formation can be described by the ramp model. However, affected by the different palaeogeomorphology gradient, the strata near the unconformity of the fourth Member of Dengying Formation has the strongest karstification and easy to develop cav-erns, breccia and mudstone filling. The horizone-phreatic zone and deep-slow-flowing zone are the main part of the karst ver-tical zonation. The strata near the unconformity of the second Member of Dengying Formation has a relatively slow karstifica-tion, with the small size of the dolomite breccia, dolomite as its cave fillings, and mainly develop vertical vadose zone, hori-zone-phreatic zone and deep-slow-flowing zone.

关键词

风化壳古岩溶/古岩溶结构/古岩溶模式/上震旦统/灯影组/四川盆地

Key words

weathering paleo-karst/paleo-karst structure/paleo-karst models/Upper Sinian/Dengying Formation/Sichuan Basin

分类

能源科技

引用本文复制引用

罗贝维,贾承造,魏国齐,杨威,谢武仁,许海龙..四川盆地上震旦统灯影组风化壳古岩溶特征及模式分析[J].中国石油大学学报(自然科学版),2015,(3):8-19,12.

基金项目

国家科技重大专项(2011ZX05007-002) (2011ZX05007-002)

中国石油大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1673-5005

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