Wilson cycle passive margins: Control of orogenic inheritance on continental breakup
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文摘

Thermo-mechanical models of rifting and breakup of orogenic lithosphere

Pre-rift crustal thickness as a control on passive margin melt productivity

Mantle exhumation due to buoyant flow of fossil mantle wedge upon extension

Inherited serpentinite rather than syn/post-rift serpentinization

Lower crustal bodies explained as preserved fossil slab or mantle wedge material

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