2010•Dizhi lunpingRequires access

Cambrian Sequence Stratigraphic Framework in Tarim Basin

Zhao Zong-ju

Open publisher page 22 citations

Abstract

Synthesizing the sequences characteristics of outcrop,drilling log and seismic data,the 3rd order sequence stratigraphic framework of Cambrian in Tarim basin has been established,and the Cambrian can be divided into six 3rd order sequences tracing and correlating in whole Tarim basin. Contrasting and analyzing between carbon isotope cycles of whole rock reflecting global sea level change or eustatic change and sedimentary cycles reflecting depositional water depth,the 3rd order sequences of Cambrian in Tarim basin may be divided into 2 types as eustatic sequence (sequence CSQ2,CSQ4,CSQ5,CSQ6),of which formation chiefly controlled by eustatic change,and tectonic sequence (sequence CSQ1,CSQ3),of which formation chiefly controlled by regional tectonic subsidence. The Cambrian platform margin in Lunnan area,northern Tarim basin,was generally behaved as evolution from ramp in Early Cambrian to rimmed platform in Middle—Late Cambrian,and progradational stacking style from west to east,it's speculated mainly related to faint eustatic fall in Cambrian and general stable and little tectonic subsidence in Tarim basin.

About this research paper

What this paper is about

Synthesizing the sequences characteristics of outcrop,drilling log and seismic data,the 3rd order sequence stratigraphic framework of Cambrian in Tarim basin has been established,and the Cambrian can be divided into six 3rd order sequences tracing and correlating in whole Tarim basin. Contrasting and analyzing between carbon isotope cycles of whole rock reflecting global sea level change or eustatic change and sedimentary cycles reflecting depositional water depth,the 3rd order sequences of Cambrian in Tarim basin may be divided into 2 types as eustatic sequence (sequence CSQ2,CSQ4,CSQ5,CSQ6),of which formation chiefly controlled by eustatic change,and tectonic sequence (sequence CSQ1,CSQ3),of which formation chiefly controlled by regional tectonic subsidence. The Cambrian platform margin in Lunnan area,northern Tarim basin,was generally behaved as evolution from ramp in Early Cambrian to rimmed platform in Middle—Late Cambrian,and progradational stacking style from west to east,it's speculated mainly related to faint eustatic fall in Cambrian and general stable and little tectonic subsidence in Tarim basin.

Why it matters

OpenAlex reports 22 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Synthesizing the sequences characteristics of outcrop,drilling log and seismic data,the 3rd order sequence stratigraphic framework of Cambrian in Tarim basin has been established,and the Cambrian can be divided into six 3rd order sequences tracing and correlating in whole Tarim basin. Contrasting and analyzing between carbon isotope cycles of whole rock reflecting global sea level change or eustatic change and sedimentary cycles reflecting depositional water depth,the 3rd order sequences of Cambrian in Tarim basin may be divided into 2 types as eustatic sequence (sequence CSQ2,CSQ4,CSQ5,CSQ6),of which formation chiefly controlled by eustatic change,and tectonic sequence (sequence CSQ1,CSQ3),of which formation chiefly controlled by regional tectonic subsidence. The Cambrian platform margin in Lunnan area,northern Tarim basin,was generally behaved as evolution from ramp in Early Cambrian to rimmed platform in Middle—Late Cambrian,and progradational stacking style from west to east,it's speculated mainly related to faint eustatic fall in Cambrian and general stable and little tectonic subsidence in Tarim basin.

Key concepts: Geology, Paleontology, Sequence (biology), Sedimentary depositional environment, Structural basin, Outcrop, Sedimentary rock, Tectonics

Related papers

Back to paper searchBrowse research topicsOriginal source
Cambrian Sequence Stratigraphic Framework in Tarim Basin — Research Paper | ScholarLens