Magmatism along strike-slip faults
id:
magmatism-along-strike-slip-faults-185-13449596
title:
Magmatism along strike-slip faults
text:
Magmatism along strike-slip faults is the process of rock melting, magma ascent and emplacement, associated with the tectonics and geometry of various strike-slip settings, most commonly occurring along transform boundaries at mid-ocean ridge spreading centres and at strike-slip systems parallel to oblique subduction zones. Strike-slip faults have a direct effect on magmatism. They can either induce magmatism, act as a conduit to magmatism and magmatic flow, or block magmatic flow. In contrast,
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wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Magmatism_along_strike-slip_faults
date created:
2023-10-09T13:13:08Z
date modified:
2024-09-07T21:07:54Z
main entity:
{"identifier":"Q123455506","url":"https://www.wikidata.org/entity/Q123455506"}
image:
fields total:
13
integrity:
14