2005Unpublished venueRequires access

GENESIS AND GEOLOGICAL CHARACTERISTICS OF THE GRANITIC BATHOLITHS IN EAST QILIAN OROGENY

Yanjie Zhang, Deng Ya-ping

Open publisher page 0 citations

Abstract

The granitic batholiths are divided into 2 instrusive sequences.They expose between Huajia mountain and Zhangjiachuan area,the eastest section of Qilian orogenic zone.The Ⅰ Period instrusive batholiths resulted from the volcanic arc evironment that was associated with ocean plates dive during Caledonia.It is calc-alklic in composition and changes in mineral components,the other resulted from superposition orogeny within land during Indosinian,it is high K-alklic in composition and changes in mineral constructures.The magmatism in the area was associated with the process that includes tectonic plates diving,collosure and superposition orogeny within land.

About this research paper

What this paper is about

The granitic batholiths are divided into 2 instrusive sequences.They expose between Huajia mountain and Zhangjiachuan area,the eastest section of Qilian orogenic zone.The Ⅰ Period instrusive batholiths resulted from the volcanic arc evironment that was associated with ocean plates dive during Caledonia.It is calc-alklic in composition and changes in mineral components,the other resulted from superposition orogeny within land during Indosinian,it is high K-alklic in composition and changes in mineral constructures.The magmatism in the area was associated with the process that includes tectonic plates diving,collosure and superposition orogeny within land.

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

The granitic batholiths are divided into 2 instrusive sequences.They expose between Huajia mountain and Zhangjiachuan area,the eastest section of Qilian orogenic zone.The Ⅰ Period instrusive batholiths resulted from the volcanic arc evironment that was associated with ocean plates dive during Caledonia.It is calc-alklic in composition and changes in mineral components,the other resulted from superposition orogeny within land during Indosinian,it is high K-alklic in composition and changes in mineral constructures.The magmatism in the area was associated with the process that includes tectonic plates diving,collosure and superposition orogeny within land.

Key concepts: Batholith, Orogeny, Geology, Geochemistry, Tectonics, Magmatism, Volcano, Earth science

Related papers

Back to paper searchBrowse research topicsOriginal source
GENESIS AND GEOLOGICAL CHARACTERISTICS OF THE GRANITIC BATHOLITHS IN EAST QILIAN OROGENY — Research Paper | ScholarLens