Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (2): 374-388.doi: 10.13278/j.cnki.jjuese.201502104

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Contraction and Extension in Nenjiang-Heihe Tectonic Belt: Evidence from the Late Paleozoic Granitoid Geochemistry

Wang Yan1, Fu Junyu1, Yang Fan1, Na Fuchao1, Chen Huijun1, Zhang Yu2, Yang Xiaoping3, Zhang Tiean2   

  1. 1. Shenyang Institute of Geology and Mineral Resources/Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China;
    2. Heilongjiang Province Institute of Regional Geology Survey, Harbin 150080, China;
    3. Qiqihar Branch, Heilongjiang Research Insitute of Geological Survey, Harbin 150036, China
  • Received:2014-06-15 Published:2015-03-26

Abstract:

We present the geochemical characteristics of the Late Paleozoic granitoid in Heilongjiang Nenjiang-Heihe through the study on the different types of granitoid. The isotopic dating results provide three time periods for these granitoids: Early Carboniferous,Late Carboniferous, and Early Permian.The granitoids are rich in silica, potassium, and sodium;and also the rare-earth elements relatively with significant negative Eu anomaly. The trace elements are typically rich in large ion lithophile element (LILE)K, Rb, Th, but poor with high-field-strength element (HFSE) Nb, P, Ti. The existence of granitic mylonite reflects its deformation and metamorphism through tuctile shear. Based on the above, the Carboniferous granitoid experienced a continental margi arc syn-collision; while the Permian granites deformed under a post-orogenesis These two reflects anenvironmental transition from a tectonic collision to an intraplate post-orgenesis, and also the activity history of genesis, convergece, andextension of the Nenjiang-Heihe tectonic belt.

Key words: granitoid, geochemistry, Late Paleozoic, Nenjiang-Heihe tectonic belt

CLC Number: 

  • P588.12

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