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海相碳酸盐台地含钾层段旋回地层学响应和识别--以川中广安地区三叠系为例

龚大兴 周家云 陈科贵 李春梅 李萌

高校地质学报Issue(2):230-238,9.
高校地质学报Issue(2):230-238,9.

海相碳酸盐台地含钾层段旋回地层学响应和识别--以川中广安地区三叠系为例

Identification of the Potassium-rich Member in Carbonate Platform and Its Response to the Gamma Ray Well Logging from the Perspective of Cyclostratigraphy:A Case Study in Triassic of Guangan Area, in the Central Sichuan Basin

龚大兴 1周家云 1陈科贵 2李春梅 2李萌3

作者信息

  • 1. 中国地质科学院 矿产综合利用研究所,成都 610041
  • 2. 西南石油大学,成都 610500
  • 3. 中国石油天然气股份有限公司 勘探开发研究院,北京 100083
  • 折叠

摘要

Abstract

To identify favorable salt-and potash-forming layer, we mainly rely on logging interpretation and coring verification. The continuously carbonate platform shows cyclical growing and recorded valuable information about the facies transition of carbonate rocks, which was synchronized with the relative sea-level cycles. This paper presents a method to preliminarily judge favorable potassium-rich intervals. By using natural gamma ray logging data and numerical simulation, high-frequency sedimentary cycles could be identified effectively from the sedimentary record. Then, we can inverse the distribution model and stacking patterns of these cycles, restore the ancient relative sea-level trends, and finally deduce the favorable salt-and potash-forming phases from the low-stand depositional system. On the basis of these principles, a case study has been taken in the Triassic strata of the Guang’an area, in the central Sichuan Basin. Our result show that the interval between the Fifth Member of the Jialingjiang Formation to the First Member of the Leikoupo Formation is the most potential salt-and potash-forming layer, which is consistent with the potassium-rich layer recognized in the drill cores. It shows that this method could effectively identify potassium rich layer from the marine carbonate platform.

关键词

海相碳酸盐岩台地/沉积旋回/含钾层段/测井响应/三叠系/川中地区

Key words

marine carbonate platform/depositional cycles/potassium-rich layer/well logging response/triassic/sichuan basin

分类

天文与地球科学

引用本文复制引用

龚大兴,周家云,陈科贵,李春梅,李萌..海相碳酸盐台地含钾层段旋回地层学响应和识别--以川中广安地区三叠系为例[J].高校地质学报,2014,(2):230-238,9.

基金项目

国家973项目“中国陆块海相成钾规律及预测研究”(2011CB403000);国家自然科学基金(41102060)资助 ()

高校地质学报

OA北大核心CSCDCSTPCD

1006-7493

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