Dynamics of intraoceanic subduction initiation: 1. Oceanic detachment fault inversion and the formation of supra-subduction zone ophiolites
نویسندگان
چکیده
منابع مشابه
Dynamics of intraoceanic subduction initiation: 1. Oceanic detachment fault inversion and the formation of suprasubduction zone ophiolites
Subduction initiation is a critical link in the plate tectonic cycle. Intraoceanic subduction zones can form along transform faults and fracture zones, but how subduction nucleates parallel to mid-ocean ridges, as in e.g., the Neotethys Ocean during the Jurassic, remains a matter of debate. In recent years, extensional detachment faults have been widely documented adjacent to slow-spreading and...
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ژورنال
عنوان ژورنال: Geochemistry, Geophysics, Geosystems
سال: 2015
ISSN: 1525-2027
DOI: 10.1002/2015gc005746