2013Journal of Oil and Gas TechnologyRequires access

Study on Sedimentary Facies of Xiaganchaigou Formation in Nanbaxian Area of Northern Qaidam Basin

Sun Hu-fa

Open publisher page 0 citations

Abstract

By researching the date of core and drilling and well logging,it was considered that the sedimentary facies,such as delta and lake facies were developed in Xiaganchaigou Formation of Nanbaxian Area.The two facies could be subdivided into distributary channel,natural barrier,inter-distributary bay,crevasse splay,underwater distributary channel,underwater inter-distibutary area,channel mouth bar,distal bar-sand sheet,delta front,predelta and shore shallow lake.Sedimentary evolution of the formation was separated into two stages.One was the lower segment(E 1 3),the other was the upper segment(E 2 3).In E 1 3 the area mainly developed shore shallow lake and distal bar-sand sheet.Sand body was at low development degree.In E 2 3,water became shallow,provenance was moved forward from northeast to south-west.Sand body is abnormally developed,delta and shore shallow lake deposit is multistage superposition.The delta front facies is especially well developed.

About this research paper

What this paper is about

By researching the date of core and drilling and well logging,it was considered that the sedimentary facies,such as delta and lake facies were developed in Xiaganchaigou Formation of Nanbaxian Area.The two facies could be subdivided into distributary channel,natural barrier,inter-distributary bay,crevasse splay,underwater distributary channel,underwater inter-distibutary area,channel mouth bar,distal bar-sand sheet,delta front,predelta and shore shallow lake.Sedimentary evolution of the formation was separated into two stages.One was the lower segment(E 1 3),the other was the upper segment(E 2 3).In E 1 3 the area mainly developed shore shallow lake and distal bar-sand sheet.Sand body was at low development degree.In E 2 3,water became shallow,provenance was moved forward from northeast to south-west.Sand body is abnormally developed,delta and shore shallow lake deposit is multistage superposition.The delta front facies is especially well developed.

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

By researching the date of core and drilling and well logging,it was considered that the sedimentary facies,such as delta and lake facies were developed in Xiaganchaigou Formation of Nanbaxian Area.The two facies could be subdivided into distributary channel,natural barrier,inter-distributary bay,crevasse splay,underwater distributary channel,underwater inter-distibutary area,channel mouth bar,distal bar-sand sheet,delta front,predelta and shore shallow lake.Sedimentary evolution of the formation was separated into two stages.One was the lower segment(E 1 3),the other was the upper segment(E 2 3).In E 1 3 the area mainly developed shore shallow lake and distal bar-sand sheet.Sand body was at low development degree.In E 2 3,water became shallow,provenance was moved forward from northeast to south-west.Sand body is abnormally developed,delta and shore shallow lake deposit is multistage superposition.The delta front facies is especially well developed.

Key concepts: Facies, Geology, Mouth bar, Delta, Shore, Sedimentary rock, Geomorphology, Provenance

Related papers

Back to paper searchBrowse research topicsOriginal source
Study on Sedimentary Facies of Xiaganchaigou Formation in Nanbaxian Area of Northern Qaidam Basin — Research Paper | ScholarLens