2009•Zhongguo dizhiRequires access

Geochemical characteristics and tectonic significance of Qixianian volcanic rocks in Zhigengaka area,Zhiduo County,eastern Qiangtang

Duan Qi-fa

Open publisher page 4 citations

Abstract

Qixianian volcanic rocks in Zhigengaka area consist of pyroclastic rocks and lava.Geochemical researches on major elements,trace elements and Sr,Nd,Pb isotopes suggest that these volcanic rocks originated from the mantle in an extension or fresh rift basin environment on the continental margin and were induced by mantle plume upwelling.On the basis of major elements,the volcanic rocks can be divided into two types characterized respectively by high TiO2 and low TiO2.Chondrite normalized REE patterns show light REE enrichment,with MORB normalized trace elements like the pig back,indicating that these volcanic rocks were formed in an intra-continental rift environment.Sr,Nd,Pb isotopic geochemistry suggests that they were derived from a depleted mantle source.

About this research paper

What this paper is about

Qixianian volcanic rocks in Zhigengaka area consist of pyroclastic rocks and lava.Geochemical researches on major elements,trace elements and Sr,Nd,Pb isotopes suggest that these volcanic rocks originated from the mantle in an extension or fresh rift basin environment on the continental margin and were induced by mantle plume upwelling.On the basis of major elements,the volcanic rocks can be divided into two types characterized respectively by high TiO2 and low TiO2.Chondrite normalized REE patterns show light REE enrichment,with MORB normalized trace elements like the pig back,indicating that these volcanic rocks were formed in an intra-continental rift environment.Sr,Nd,Pb isotopic geochemistry suggests that they were derived from a depleted mantle source.

Why it matters

OpenAlex reports 4 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

Qixianian volcanic rocks in Zhigengaka area consist of pyroclastic rocks and lava.Geochemical researches on major elements,trace elements and Sr,Nd,Pb isotopes suggest that these volcanic rocks originated from the mantle in an extension or fresh rift basin environment on the continental margin and were induced by mantle plume upwelling.On the basis of major elements,the volcanic rocks can be divided into two types characterized respectively by high TiO2 and low TiO2.Chondrite normalized REE patterns show light REE enrichment,with MORB normalized trace elements like the pig back,indicating that these volcanic rocks were formed in an intra-continental rift environment.Sr,Nd,Pb isotopic geochemistry suggests that they were derived from a depleted mantle source.

Key concepts: Geology, Geochemistry, Volcanic rock, Pyroclastic rock, Rift, Lava, Volcano, Mantle plume

Related papers

Back to paper searchBrowse research topicsOriginal source
Geochemical characteristics and tectonic significance of Qixianian volcanic rocks in Zhigengaka area,Zhiduo County,eastern Qiangtang — Research Paper | ScholarLens