| China Geological Survey Chinese Academy of Geological Sciences | Host |
| 科学出版社 | Publish |
| Citation: |
SONG Yucai, HOU Zengqian, LIU Yingchao, ZHANG Hongrui. 2017. Mississippi Valley-Type (MVT) Pb-Zn deposits in the Tethyan domain:A review[J]. Geology in China, 44(4): 664-689. doi: 10.12029/gc20170403
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Mississippi Valley-Type (MVT) Pb-Zn deposits in the Tethyan domain:A review
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Abstract
The Tethyan domain hosts the world's most abundant Mississippi Valley-Type (MVT) Pb-Zn deposits, which occur in fold-thrust belts and forelands on both sides of the continent-continent collisional zone through the whole Tethyan domain. Mineralization commonly took place when the ore districts were experiencing strike-slip or extensional deformation, which occurred after regional compression or during the late stage of a compressional deformation event. The main ore-controlling factors include extensional faults, evaporite diapir, carbonate dissolution and collapse, evaporite dissolution and collapse, porous dolostone, and barite-bearing strata. Records of hydrocarbon fluids are present in many Pb-Zn deposits and ore districts of the Tethyan domain. They reacted with (dissolved) sulfate to provide reduced sulfur for the ore formation. The generation of such abundant MVT Pb-Zn deposits in the Tethyan domain can be attributed to the continent-continent collisional tectonic setting, large amounts of evaporites, and plentiful hydrocarbon fluids. This study raises the exploration potential for MV TPb-Zn deposits in the Tethyan domain.
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SONG Yucai, HOU Zengqian, LIU Yingchao, ZHANG Hongrui. 2017. Mississippi Valley-Type (MVT) Pb-Zn deposits in the Tethyan domain:A review[J]. Geology in China, 44(4): 664-689. doi: 10.12029/gc20170403
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- Figure 1. Distribution of Mississippi Valley-type (MVT) lead–zinc deposits in the Tethyan domain (background map after http://www.maps-for-free.com/)
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Figure 2.
a-Top 30 Mississippi Valley-type (MVT) lead-zinc deposits in the world (based on data from Table 1 and Taylor et al., 2009; this ranking is regardless of category of resources); b-Top 30 Mississippi Valley-type (MVT) lead-zinc deposits in the Tethyan domain (based on data from Table 1; this ranking is regardless of category of resources)
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Figure 3.
Simplified geological cross-sections through some important collisional orogens in the Tethyan domain and distribution of Mississippi Valley-type (MVT) lead–zinc deposits (a, modified after Li et al., 2015; b, modified after Mouthereau et al., 2012; c, based on Zhang and Hou, 2015 modified after Dal Piaz et al., 2003; d, modified after Verges et al., 2002; e, modified after Bouhlel et al., 2016. See locations of the geological cross-sections legends for deposits in Fig. 1)