Ancient deep roots for Mesozoic world-class gold deposits in the north
China craton: An integrated genetic perspective
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Abstract
The North China Craton (NCC) hosts some of the world-class gold deposits that formed more than 2
billion years after the major orogenic cycles and cratonization. The diverse models for the genesis of
these deposits remain equivocal, and mostly focused on the craton margin examples, although synchronous
deposits formed in the interior domains. Here we adopt an integrated geological and
geophysical perspective to evaluate the possible factors that contributed to the formation of the major
gold deposits in the NCC. In the Archean tectonic framework of the NCC, the locations of the major gold
deposits fall within or adjacent to greenstone belts or the margins of micro-continents. In the Paleoproterozoic
framework, they are markedly aligned along two major collisional sutures e the Trans North
China Orogen and the Jiao-Liao-Ji Belt. Since the Mesozoic intrusions hosting these deposits do not carry
adequate signals for the source of gold, we explore the deep roots based on available geophysical data.
We show that the gold deposits are preferentially distributed above zones of uplifted MOHO and shallow
LAB corresponding to thinned crust and eroded sub-lithospheric mantle, and that the mineralization is
located above regions of high heat flow representing mantle upwelling. The NCC was at the center of a
multi-convergent regime during the Mesozoic which intensely churned the mantle and significantly
enriched it. The geophysical data on Moho and LAB upwarp from the centre towards east of the craton is
more consistent with paleo-Pacific slab subduction from the east exerting the dominant control on
lithospheric thinning. Based on these results, and together with an evaluation of the geochemical and
isotopic features of the Mesozoic magmatic intrusions hosting the gold mineralization, we propose a
genetic model that invokes reworking of ancient Au archives preserved in the lower crust and metasomatised
upper mantle and which were generated through multiple subduction, underplating and
cumulation events associated with cratonization of the NCC as well as the subduction-collision of
Yangtze Craton with the NCC. The heat and material input along zones of heterogeneously thinned
lithosphere from a rising turbulent mantle triggered by Mesozoic convergent margins surrounding the
craton aided in reworking the deep roots of the ancient Au reservoirs, leading to the major gold metallogeny
along craton margins as well as in the interior of the NCC.
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