2021, 40(1) 29-40 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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Keywords
 LA - ICP - MS zircon U - Pb dating
Lu - Hf isotopes
petrogeochemistry
Yuejinshan coppergold
deposit
Authors
WANG Chong-yi
HAO Yu-jie
SHANG Qing-qing
SHI Yu-fan
GAO Yu
REN Yun-sheng
PubMed
Article by Wang C
Article by Hao Y
Article by Shang Q
Article by Shi Y
Article by Gao Y
Article by Ren Y

 Chronological and geochemical characteristics of granodiorite from Yuejinshan skarn - type copper - gold deposit in Heilongjiang Province

 

 1. College of Earth Sciences,Jilin University,Changchun 130061,China;

2. College of Earth Sciences,Institute of Disaster Prevention,Sanhe 065201,Hebei,China

Abstract

 The LA - ICP - MS zircon U - Pb dating and Lu - Hf isotopic analyses as well as whole-rock geochemistry study were carried on the granodiorite related to skarn mineralization in Yuejinshan copper-gold deposit.The results show that the weighted average age of 206Pb /238U of 26 zircon points in the granodiorite is ( 118. 96 ±0. 77) Ma ( MSWD = 0. 29) . The εHf

( t) values of zircons in the rock mass are all positive ( + 1. 4 ~ + 3. 2) ,with young Hf two-stage model age ( TDM2 = 1. 09 ~ 0. 98 Ga) . Geochemically,the granodiorite is rich in Al,K,
Na,and depleted in Ti,P,Ca,indicating calcium alkaline I-type granite. For rare earth elements ( REE) composition,the granodiorite is enriched in light REE and depleted in heavy REE. Combined with the low positive εHf
( t) values,it is indicated that the magma is from a mixing source between crust and mantle. Based on the petrogeochemical mapping and the evolution of the regional tectonic background,both the granodiorite and granite porphyry belong to post-collision volcanic arc granites. The metallogenic diagenesis of the study area is directly related to the lower lithosphere mantle delamination under the tectonic environment of intense subduction of the Paleo - Pacific
Ocean plate.

Keywords  LA - ICP - MS zircon U - Pb dating   Lu - Hf isotopes   petrogeochemistry   Yuejinshan coppergold
deposit
  
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