2015, 34(1) 34-43 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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Keywords
granitic complex
zircon U- - Pb age
geochemical characteristics
Huolongmen area
Xiao Hing- gan mountains
Authors
QU Hui
LI Cheng-Lu
YANG Fu-Shen
PubMed
Article by Qu, H.
Article by Li, C. L.
Article by Yang, F. S.

Zircon U- - Pb ages��geochemical characteristics and their geological implication of granitic complex in Huolongmen area��northwestern Xiao Hinggan mountains

QU Hui, LI Cheng-Lu, YANG Fu-Shen

Heilongjiang Institute of Geological Survey��Harbin 150036��China

Abstract��

The Huolongmen area in Xiao Hinggan mountains is tectonically located in the eastern Xingmeng oregenic belt�� A large area of exposed granitic complex is an important part of the Xinkailing- -Kele complex�� The granitic complex is mainly composed of granite and granodioritic mylonite�� Dating of the zircon U- -Pb SH��IMP�� concordant age of the granitic mylonite is 310. 7 ± 6. 5 Ma�� implying that their protolith formed in the Late Carbon- iferous�� Major elements of the granitic complex indicate medium to high potassium calc- alkaline and metaluminous to peraluminous in composition�� Trace elements demonstrate the enrichment of Th��Zr��Hf��Nd����b��K and de- pletion of Ba��Sr��Nb��P��Ti�� The samples are enriched in L��EE (light rare earth elements) and depleted in H��EE (heavy rare earth elements) with pronounced negative Eu anomalies��suggesting a high degree fractionation of L��EE and H��EE�� Based on the regional tectonic evolution characteristics and forming environment of granitic complex��we interpreted that their protolith formed in Late Paleozoic��but significant deformation and metamorphism occurred in Trassic��

Keywords�� granitic complex   zircon U- - Pb age   geochemical characteristics   Huolongmen area   Xiao Hing- gan mountains  
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