2008Unpublished venueRequires access

The sedimentary macro-facies characteristics of Xin'an village group in FangZheng fault area of YiShu graben

Dong Xiu

Open publisher page 0 citations

Abstract

According to core,seismic,well log and logging data,utilizing the principles and methods of sequence stratigraphy and sedimentology to identify the sedimentary micro-facies characteristics of Xin'an village group in Fangzheng fault area of yishu graben.The result shows that the main type of the sedimentary micro-facies developed in Xin'an village group of Fangzheng area is distributary channels,underwater distributary channels,river mouth bars,sand sheets,shore-shallow lacustrine sandy beach bar and mud bar.Along the edge of the northwest fault to the midst of the fault,it has transition from fan deltaic plain subfacies,fan deltaic front subfacies to lacustrine facies in the plane,parts of the region has developed sublacustrine fan.Along the southeast fault to the middle has developed deltaic front subfacies and lacustrine facies,deltaic facies has developed in the north and lacustrine facies developd in the south.

About this research paper

What this paper is about

According to core,seismic,well log and logging data,utilizing the principles and methods of sequence stratigraphy and sedimentology to identify the sedimentary micro-facies characteristics of Xin'an village group in Fangzheng fault area of yishu graben.The result shows that the main type of the sedimentary micro-facies developed in Xin'an village group of Fangzheng area is distributary channels,underwater distributary channels,river mouth bars,sand sheets,shore-shallow lacustrine sandy beach bar and mud bar.Along the edge of the northwest fault to the midst of the fault,it has transition from fan deltaic plain subfacies,fan deltaic front subfacies to lacustrine facies in the plane,parts of the region has developed sublacustrine fan.Along the southeast fault to the middle has developed deltaic front subfacies and lacustrine facies,deltaic facies has developed in the north and lacustrine facies developd in the south.

Why it matters

A significance statement is not available in the OpenAlex record.

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

According to core,seismic,well log and logging data,utilizing the principles and methods of sequence stratigraphy and sedimentology to identify the sedimentary micro-facies characteristics of Xin'an village group in Fangzheng fault area of yishu graben.The result shows that the main type of the sedimentary micro-facies developed in Xin'an village group of Fangzheng area is distributary channels,underwater distributary channels,river mouth bars,sand sheets,shore-shallow lacustrine sandy beach bar and mud bar.Along the edge of the northwest fault to the midst of the fault,it has transition from fan deltaic plain subfacies,fan deltaic front subfacies to lacustrine facies in the plane,parts of the region has developed sublacustrine fan.Along the southeast fault to the middle has developed deltaic front subfacies and lacustrine facies,deltaic facies has developed in the north and lacustrine facies developd in the south.

Key concepts: Facies, Geology, Graben, Sedimentology, Fault (geology), Sedimentary rock, Group (periodic table), Delta

Related papers

Back to paper searchBrowse research topicsOriginal source
The sedimentary macro-facies characteristics of Xin'an village group in FangZheng fault area of YiShu graben — Research Paper | ScholarLens