Synkinematic mafic/ultramafic sheeted intrusions: emplacement mechanism and strain restoration of the Permian Huangshan Ni-Cu ore belt (Eastern Tianshan, NW China) - INSU - Institut national des sciences de l'Univers Access content directly
Journal Articles Journal of Southeast Asian earth sciences Year : 2012

Synkinematic mafic/ultramafic sheeted intrusions: emplacement mechanism and strain restoration of the Permian Huangshan Ni-Cu ore belt (Eastern Tianshan, NW China)

Abstract

Whilst petrology, geochemistry and metal content of small mafic/ultramafic Ni-Cu bearing complexes have been extensively studied, their structural controls and emplacement mechanisms are still poorly documented. This study addresses the last two points with the Huangshan Ni-Cu ore belt (Chinese Eastern Tianshan) as a case study. The Huangshan intrusions are Early Permian; a period when the Tianshan orogenic belt recorded major right-lateral wrench tectonics, characterized by crustal-scale shear zones. Detailed mapping, petro-structural analysis and strain rate calculation within and around the intrusions allow us to establish that the Huangshan Ni-Cu-bearing mafic/ultramafic complexes are not layered intrusions. Instead, they emplaced by injection of several mafic/ultramafic magma batches within kilometre-scale tension gashes generated by Permian dextral shearing, and should be considered as synkinematic sheeted intrusions. Finite strain analysis across the Huangshan-Kangguer shear zone provides rather high shear strain rates (∼4.5). Considering the location and alignment of the Ni-Cu-bearing mafic/ultramafic bodies along regional shear zones throughout Eastern Tianshan, it appears that wrench tectonics most likely controlled and focussed the intrusion of parent magmas. As a consequence, rifting related to post-orogenic extension is not required to account for Permian magmatic features of the Tianshan Belt. Finally, the Huangshan Ni-Cu bearing mafic/ultramafic intrusions are neither parts of an ophiolitic suture, nor of a dunite-cored Alaskan-type ore deposit, as postulated in some previous studies. In the light of these new results, we believe that structural controls and emplacement mechanisms of many Ni-Cu sulphides deposits hosted by small intrusions (particularly funnel-shaped ones) should be (re-)evaluated from a structural and geophysical point of view.
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insu-00708256 , version 1 (09-07-2012)

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Yannick Branquet, Charles Gumiaux, Stanislas Sizaret, Luc Barbanson, Bo Wang, et al.. Synkinematic mafic/ultramafic sheeted intrusions: emplacement mechanism and strain restoration of the Permian Huangshan Ni-Cu ore belt (Eastern Tianshan, NW China). Journal of Southeast Asian earth sciences, 2012, 56, pp.240-257. ⟨10.1016/j.jseaes.2012.05.021⟩. ⟨insu-00708256⟩
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