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SUN Zhuanrong, DONG Guochen, ZHAO Zuoxin, WANG Weiqing, LIU Shengqiang. 2017. Petrological, geochemical and geochronological features of Lailishan ganitoids in western Yunnan and their genesis of partial melting of crustal soure[J]. Geology in China, 44(6): 1140-1158. doi: 10.12029/gc20170608
Citation: SUN Zhuanrong, DONG Guochen, ZHAO Zuoxin, WANG Weiqing, LIU Shengqiang. 2017. Petrological, geochemical and geochronological features of Lailishan ganitoids in western Yunnan and their genesis of partial melting of crustal soure[J]. Geology in China, 44(6): 1140-1158. doi: 10.12029/gc20170608
shu

Petrological, geochemical and geochronological features of Lailishan ganitoids in western Yunnan and their genesis of partial melting of crustal soure

  • 1.

    School of Earth Science and Resources, China University of Geosciences(Beijing), Beijing 100083, China

  • 2.

    Exploration Institute of Geology and Mineral Resources of Yunnan, Kunming 650011, Yunnan, China

    • Fund Project: Supported by National Key Projects for Basic Research of China (No. 2015CB452604) and Prospecting Program for Tengliang Tin Mineralized Belt (No. 12120114013801)
More Information
  • Author Bio: SUN Zhuanrong, female, born in 1994, doctor candidate, majors in mineralogy, petrology and mineral deposits; E-mail:834992943@qq.com
  • Corresponding author: DONG Guochen, male, born in 1962, professor, supervisor of doctor candidates, engages in the study of petrology and mineral deposits; E-mail:donggc@cugb.edu.cn 
Received Date:  21 January 2016
Revised Date:  05 April 2016
Publish Date:  25 December 2017
    Abstract

  • Granites genetically related to tin ore deposits always constitute the focus of geological studies. The Lailishan granitoids are located in the Tengchong-Lianghe area of western Yunnan and belong tectonically to Tengliang granitoids. These granites extend in NNE direction as a belt, connected with Gangdise belt on the north. The Lailishan granitoids are mainly composed of porphyaceous biotite monzogranite and medium to coarse-grained biotite syenogranite. Based on the data available, the authors conducted petrological, geochemical and geochronological studies of the Lailisahn granitoids. The zircon LA-ICP-MS U-Pb age of the monzogranite (14L-4) is 52.34 ±0.68Ma (MSWD=1.4, n=26). Geochemically, the monzogranite is relatively rich in Al (Al2O3=14.70%-15.27%), alkalis (K2O+Na2O=8.07%-8.50%), Ca (CaO=1.64%-2.56%), REE, and Ba. The ASI values range from 0.97 to 1.12, 1.04 on average, indicating that monzogranite is from metaluminous to weakly peraluminous. The syenogranite is relatively rich in Si (SiO2=74.57%-76.69%) and Rb, and strongly depleted in Ba, Sr, P, Ti, and Eu. The ASI values range from 1.05 to 1.18, 1.09 on average, indicating weakly peraluminous features. The monzogranite and syenogranite originated from the same magma reservoir but emplaced at different stages; the evolution of them in mineralogy, geochemistry and chronology was obvious, suggesting S-type granites. It is therefore held that the Lailishan granitoids originated from crust partial melting in deep crust during main Indian-Euro-Asian collision period, responding to the interaction between the Indian-Euro-Asian continents.

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