High resolution chemical sequence stratigraphy analysis of Wufeng Formation and Lower Longmaxi Formation in the Well Xindi 1, Upper Yangtze region

WANG Qian; HUANG Yongjian; ZHANG Zhifeng; WANG Changhong; LI Xiang; LIU Wei

doi:10.12029/gc20200906001

GEOLOGY IN CHINA > 2024 > 51(4): 1355-1367. > DOI: 10.12029/gc20200906001

Wang Qian, Huang Yongjian, Zhang Zhifeng, Wang Changhong, Li Xiang, Liu Wei. 2024. High resolution chemical sequence stratigraphy analysis of Wufeng Formation and Lower Longmaxi Formation in the Well Xindi 1, Upper Yangtze region[J]. Geology in China, 51(4): 1355−1367. DOI: 10.12029/gc20200906001

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High resolution chemical sequence stratigraphy analysis of Wufeng Formation and Lower Longmaxi Formation in the Well Xindi 1, Upper Yangtze region

1.
Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
3.
Chengdu Center, China Geological Survey, Chengdu 610082, Sichuan, China

Funds: Supported by National Science and Technology Major Project (No.2016ZX05029-001).

More Information

Author Bio:
WANG Qian, female, born in 1990, doctor, engaged in sedimentology and geochemistry; E-mail: 944085175@qq.com
Corresponding author:
HUANG Yongjian, male, born in 1974, doctor, associate professor, engaged in sedimentology and geochemistry; E-mail: haungyj@cugb.edu.cn.
Received Date: September 05, 2020
Revised Date: December 12, 2020

Graphical Abstract

Abstract

Abstract

This paper is the result of geological survey engineering.
Objective
The purpose of this paper is to synthesize the theories and methods of comprehensive geochemistry and high resolution sequence stratigraphy. The high−precision chemical sequence stratigraphic framework of Wufeng Formation and Lower Longmaxi Formation in Xindi 1 Well, Upper Yangtze region was established to provide scientific basis for shale gas exploration in the study area.
Methods
We use the core, logging and sample analysis data of Well Xindi 1 in Upper Yangtze region to optimize the indicators system which can divide the chemical sequence stratigraphic. The indicators system contains three elements assemblages: the terrigenous input intensity(TII), the autogenetic precipitation intensity(API), and the organic matter adsorption and deoxidation intensity(ODI). Then the fourth−order chemical sequence stratigraphy is divided by these three elements assemblages.
Results
Based on the above indicators system, Wufeng Formation of Liutang section is divided into LCW sequence, the lower part of Longmaxi Formation is divided into MCL1−1, MCL1−2, MCL1−3, MCL1−4 fourth−order sequences upwardly. The total amount of elements assemblages related to TII is relatively high near the sequence boundary, but relatively low near the maximum oceanic flooding surface. However, the total amount of element assemblages related to API and ODI are generally lower near the sequence boundary and higher near the maximum flooding surface.
Conclusions
Representing different genetic significance, the cyclic variation of element assemblages is respond to regional sea level change, and has regional consistency. The sedimentary environment with smaller TII, smaller API and larger ODI is conducive to organic matter enrichment in shale. So it can be used as the basis for regional stratigraphic correlation.
- Upper Yangtze region,
- Well Xindi 1,
- Wufeng Formation,
- Longmaxi Formation,
- chemical sequence stratigraphy,
- geological survey engineering
Highlights
A new idea of chemical sequence stratigraphy in the development of isochronous fine division and correlation of shale segments is explored. A theoretical model of chemical sequence stratigraphy based on the combination of geochemical elements of different origin is established.

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References (64)

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High resolution chemical sequence stratigraphy analysis of Wufeng Formation and Lower Longmaxi Formation in the Well Xindi 1, Upper Yangtze region