Zircon U-Pb Dating and Geochemical Characteristics of Sihaiping Pluton from Southern Qinling Orogenic Belt in Shaanxi

CHEN Qingmin; GUO Qiming; WANG Qiang; WANG Zhe; ZHANG Shuanhou

Northwestern Geology > 2017 > 50(3): 65-73.

CHEN Qingmin, GUO Qiming, WANG Qiang, et al. Zircon U-Pb Dating and Geochemical Characteristics of Sihaiping Pluton from Southern Qinling Orogenic Belt in Shaanxi[J]. Northwestern Geology, 2017, 50(3): 65-73.

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Zircon U-Pb Dating and Geochemical Characteristics of Sihaiping Pluton from Southern Qinling Orogenic Belt in Shaanxi

Shaanxi Center of Geological Survey, Xi'an 710068, Shaanxi, China

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Received Date: January 09, 2017
Revised Date: April 22, 2017
Available Online: July 28, 2022
Published Date: September 04, 2017

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Abstract

Based on the geology, petrology and geochemistry studies, off whitemedium-granule-biotite-adamellite and porphyritic biotite-adamellite from the Sihaiping intrusion were identified. The Sihaipinggranitoid belongs to high-K calc-alkaline serieswith aluminous-peraluminous characteristics, which was enriched in Rb, Th, K and Nd,depleted in Ba, Nb, Ta, La, P and Eu, with significant loss of Nb, Ta and P. In addition, this intrusion has moderate-low REE concentration and right deviated distribution curve. It suggests that Sihaiping granite mass might be formed in aintra-plate setting.The magma came from the partial melting of earth crust. LA-ICP-MS zircon U-Pb analysis suggested that Sihaiping intrusion was formed at 168.2±1.1Ma, which is later than U-Pb age of Yanzhiba intrusion. Combining with previous researches, Sihaiping-Yanzhiba intrusions had experienced several magmation from late Triassic to middle Jurassic.
- Sihaiping granitoid,
- geochemistry,
- LA-ICP-MS zircon U-Pb dating

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Zircon U-Pb Dating and Geochemical Characteristics of Sihaiping Pluton from Southern Qinling Orogenic Belt in Shaanxi

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