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2019 Vol. 46, No. 6
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XIE Jihai, HU Zhengxiang, MAO Xinwu, KONG Lingyao, YANG Qingxiong, YANG Cheng, GUO Pan. 2019. The discrimination of Jinningian MORB-like basalt and intra-oceanic subduction in the Dahongshan area, Northern Hubei[J]. Geology in China, 46(6): 1496-1511. doi: 10.12029/gc20190616
Citation: XIE Jihai, HU Zhengxiang, MAO Xinwu, KONG Lingyao, YANG Qingxiong, YANG Cheng, GUO Pan. 2019. The discrimination of Jinningian MORB-like basalt and intra-oceanic subduction in the Dahongshan area, Northern Hubei[J]. Geology in China, 46(6): 1496-1511. doi: 10.12029/gc20190616
shu

The discrimination of Jinningian MORB-like basalt and intra-oceanic subduction in the Dahongshan area, Northern Hubei

  • 1.

    Wuhan Geomatics Institute, Wuhan 430034, Hubei, China

  • 2.

    Hubei Geological Survey, Wuhan 430034, Hubei, China

    • Fund Project: Supported by Hubei Geological Bureau Science and Technology Project (No. KJ2019-2) and China Geological Survey Program (No. 12120113012800)
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  • Author Bio: XIE Jihai, male, born in 1976, senior engineer, majors in hydrogeology and engineering geology, engages in urban geological survey, prevention and cure of geological hazard, geotechnical engineering and technical management; E-mail: 51344552@qq.com
  • Corresponding author: HU Zhengxiang, male, born in 1963, professor, majors in geological and mineral exploration, engages in geological and mineral investigation and technical management; ;E-mail:1113153933@qq.com 
Received Date:  13 February 2018
Revised Date:  25 March 2019
Publish Date:  25 December 2019
    Abstract

  • There are numerous mafic rocks e.g., gabbro, diabase, basalt, pillow basalt, fumarolic-amygdaloidal basalt, in the Dahongshan area, Suizhou City, northern Hubei Province. They are mainly in the form of block structurally mixed in a set of clastic rock, characterized by mélange of exotic blocks and matrix strata, suggesting a typical orogenic belt. The mafic rocks from Dahongshan area show the features of tholeiite series, and are geochemically enriched in incompatible elements such as Rb, Ba, K, Th and U and depleted in high field strength elements such as Nb and Ta, similar to features of island arc basalts. Nevertheless, the features of flat REE patterns (ΣLREE/ΣHREE=1.41-4.48, LaN/YbN=0.76-4.79, Zr/Y=2.65-5.38 and Ti/V=29.19-54.97) are the same as features of mid-ocean ridge basalt. Therefore, the geochemical signatures and regional geological characteristics show that these mafic rocks should be part of MORB-like/fore-arc basalts, formed along intra-ocean arc where the subduction-initiation happened. Their parent magma was produced by the nascent depleted MORB mantle and interacted with the contribution of fluids from the slab sinking plate with decompression melting. The basalts from Nanfengya and Lulinzhai yielded LA-ICP-MS U-Pb zircon ages of (816.6±7.6) Ma (MSWD=0.47) and (813.1±4.8) Ma (MSWD=0.37) respectively, interpreted as their crystallization age. Combined with the previous research results of gabbro in Yangjiapeng (947 Ma), pillow basalt in Changhe (824 Ma), and diabase in Luling (820 Ma), it is held that mass mafic rocks were formed in Jinningian period (817-947 Ma) in the Dahongshan area. They may be the products of multi-stage intra-ocean subduction. The discrimination of Jinningian ore-arc/MORB-like basalt in the Dahongshan suggests that it experienced a certain scale of ocean-ocean to ocean-continent subduction and orogeny between Yangtze block and Tongbai-Dabie block in Jinningian period, and the two blocks might have been aggregated together in late Qingbaikou period.

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