中天山南缘乌瓦门早志留世安第斯型安山岩的发现及意义

牛晓露; 刘飞; 冯光英; 杨经绥

doi:10.3799/dqkx.2018.725

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1350-1366

Niu Xiaolu, Liu Fei, Feng Guangying, Yang Jingsui, 2018. Discovery and Significance of Early Silurian Andesites in Wuwamen Area, Southern Margin of Central Tianshan Block. Earth Science, 43(4): 1350-1366. doi: 10.3799/dqkx.2018.725

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Niu Xiaolu, Liu Fei, Feng Guangying, Yang Jingsui, 2018. Discovery and Significance of Early Silurian Andesites in Wuwamen Area, Southern Margin of Central Tianshan Block. Earth Science, 43(4): 1350-1366. doi: 10.3799/dqkx.2018.725

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Discovery and Significance of Early Silurian Andesites in Wuwamen Area, Southern Margin of Central Tianshan Block

doi: 10.3799/dqkx.2018.725

Center for Advanced Research on Mantle(CARMA), Key Laboratory of Deep-Earth Dynamics, Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

Andesite is a typical rock type in subduction-related environment, and can reveal important information on the subduction processes. In this paper, it is presented of zircon U-Pb geochronology, whole-rock major and trace element and Sr-Nd isotope data for the Wuwamen andesites in the southern margin of Central Tianshan block, to provide constraints on the evolution processes of the South Tianshan ocean and Central Tianshan block. The andesites are high-K, calc-alkaline trachyandesite composed of augite, calcic amphibole, plagioclase and K-Na feldspar, with SiO₂=56.23%-59.28%, K₂O=2.70%-3.37%, and Na₂O=3.32%-4.11%. They are characterized by fractionated rare earth element patterns with (La/Yb)_N=18.5-20.9, and show negligible Eu anomalies with δEu=0.82-0.88; they are highly enriched in Rb, Ba and Sr, and depleted in Nb, Ta and Ti. Their initial ⁸⁷Sr/⁸⁶Sr ratios are in the range of 0.706 2-0.707 5 and ε_Nd(t) in the range of 2.96-3.01. The data suggest that the Wuwamen andesites are typical Andean-type continental arcs, which originated from the partial melting of the mantle wedge that had been previously metasomatized by subduction-related fluids; the parental magma has been modified by the old crustal rocks during the magmas ascent. The origin and tectonic affinity of the Wuwamen andesites indicate that the South Tianshan ocean has subducted northward beneath the southern margin of the Central Tianshan block at the end of Early Silurian, forming a mature oceanic-continental subduction system; the southern margin of the Central Tianshan block has been a typical active continental margin characterized by development of Andean-type continental arc rocks.
- andesite,
- zircon U-Pb dating,
- geochemistry,
- Andean-type continental margin,
- South Tianshan ocean,
- Central Tianshan block

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References(83)

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