Volume 19 Issue 3
Sep.  2013
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LI Sun-xiong, WEI Chang-xin, WANG Yan-hua, et al., 2013. ACORITE U-Pb CHRONOLOGY CHARACTERISTICS AND ITS GEOLOGICAL SIGNIFICANCE OF DUCTILE SHEAR DEFORMABLE BELT IN SOUTHEASTERN HAINAN ISLAND, CHINA. Journal of Geomechanics, 19 (3): 267-274.
Citation: LI Sun-xiong, WEI Chang-xin, WANG Yan-hua, et al., 2013. ACORITE U-Pb CHRONOLOGY CHARACTERISTICS AND ITS GEOLOGICAL SIGNIFICANCE OF DUCTILE SHEAR DEFORMABLE BELT IN SOUTHEASTERN HAINAN ISLAND, CHINA. Journal of Geomechanics, 19 (3): 267-274.

ACORITE U-Pb CHRONOLOGY CHARACTERISTICS AND ITS GEOLOGICAL SIGNIFICANCE OF DUCTILE SHEAR DEFORMABLE BELT IN SOUTHEASTERN HAINAN ISLAND, CHINA

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  • Received: 2013-03-17
  • Published: 2013-09-01
  • The ductile shear belt exposures in Mangsan Reservoir-Diaoluoshan Tree Farm-Xinglong area successively with its strike being north-east. The lithology is tectonic gneiss and granite of mylonitization, and main minerals are composed of feldspar, quartz and biotite. The rock develops as "S-C" fabric, "δ" style gyral porphyroclast system, mica fish etc. The tectonic fabric indicates right handed shearing movement. According to mineral component and deforming feature, the deforming environment should be low amphibolite facies, which belongs to the product emplacing across the shear zone and transforming synchronously. This time we got 284.3±1.3 Ma and 265.9±1.3 Ma by laser ICP-MS for zircons from Mangsan Reservoir and Diaoluoshan Tree Farm. The founding of ductile shear belt and its geologic age plays an important role in the intensive study of construction-magma function of Hainan Island.

     

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  • [1]
    张业明, 谢才富, 付太安, 等.三亚地体和琼中地体构造边界的直接证据[J].科学与工程, 2005, 5(20):1482~1484. http://www.cnki.com.cn/Article/CJFDTOTAL-KXJS200520003.htm

    ZHANG Ye-ming, XIE Cai-fu, FU Tai-an, et al. The direct evidence about tectonic boundary between Sanya Terrain and Qiongzhong Terrain[J]. Science Technology and Engineering, 2005, 5(20):1482~1484. http://www.cnki.com.cn/Article/CJFDTOTAL-KXJS200520003.htm
    [2]
    李孙雄, 范渊, 莫位明, 等.海南岛古生代弧状构造带的特征及其地质意义[J].矿产与地质, 2006, 20(3):232~236. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD200603005.htm

    LI Sun-xiong, FAN Yuan, MO Wei-ming, et al. Characteristics of arc structure zones in the Paleozoic era of Hainan island, and its geological implications[J]. Mineral Resources and Geology, 2006, 20(3):232~236. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD200603005.htm
    [3]
    谢才富. 海南岛海西期同逆冲侵入岩组合的厘定及其构造意义[D]. 南京: 南京大学, 2007. http://d.wanfangdata.com.cn/Thesis/Y1435015

    XIE Cai-fu. Validation on Hercynian iso-thrusting irruptive rock assemblage in Hainan Island and its tectonic implication[D]. Nanjing:Nanjing University, 2007. http://d.wanfangdata.com.cn/Thesis/Y1435015
    [4]
    任纪舜.中国大地构造及其演化[M].北京:科学出版社, 1980.

    REN Ji-shun. Geotectonics and evolution in China[M]. Beijing:Science Press, 1980.
    [5]
    杨树锋, 虞子冶, 郭令智, 等.海南岛的地体划分、古地磁研究及其板块构造意义[J].南京大学学报:地球科学版, 1989, 1(1/2):38~46.

    YANG Shu-feng, YU Zi-ye, GUO Ling-zhi, et al. Differentiation of Hainan terrane, the research of paleogeomagnetism and the significance of plate tectonics[J]. Journal of Nanjing University:Natural Sciences Edition, 1989, 1(1/2):38~46.
    [6]
    谢才富, 朱金初, 赵子杰, 等.三亚石榴霓辉石正长岩的锆石SHRIMP U-Pb年龄:对海南岛海西-印支期构造演化的制约[J].高校地质学报, 2005, 11(1):47~57. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200501002.htm

    XIE Cai-fu, ZHU Jin-chu, ZHAO Zi-jie, et al. Zircon SHRIMP U-Pb age dating of garnet-acmite syenite:Constraints on the Hercynian-Indosinian tectonic evolution of Hainan Island[J]. Geological Journal of China Universities, 2005, 11(1):47~57. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200501002.htm
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