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Formation of the Xigaze Metamorphic Sole under the Tibetan continental margin reveals generic characteristics of the subduction initiation process

2023-03-07

Abstract excerpt

Metamorphic soles found under allochthonous oceanic lithosphere, or ophiolites, are derived from the earliest lower plate oceanic crust accreted to upper plate mantle and are considered diagnostic of intraoceanic subduction initiation. Their metamorphic evolution is inferred to reflect the thermal structure at the site of subduction nucleation, with granulite-bearing soles linked to initiation at hot spreading cen...

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Literature Corpus work
a4d4ab7a-6955-5710-85ef-3a77929b9c43
DOI
10.21203/rs.3.rs-2621281/v1
Open publication

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Formation of the Xigaze Metamorphic Sole under the Tibetan continental margin reveals generic characteristics of the subduction initiation processDOI 10.21203/rs.3.rs-2621281/v1
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