A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects

The Central Asian Orogenic Belt (CAOB) was originated from the subduction, closure, convergence, and post-collisional extension of the Paleo-Asian Ocean located between the North China Craton, Tarim Craton, and the Siberian Craton during the late Permian to early Triassic. The Magnetotelluric (MT) m...

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Autori principali:	Yifan Li, Letian Zhang, Sheng Jin, Lishui Zhou, Qiyao Zong
Natura:	Artigo
Lingua:	Inglês
Pubblicazione:	Frontiers Media S.A. 2025-01-01
Serie:	Frontiers in Earth Science
Soggetti:	magnetotellurics Central Asian Orogenic Belt Paleo-Asian Ocean lithospheric electrical structure formation mechanism of low-resistivity zones
Accesso online:	https://www.frontiersin.org/articles/10.3389/feart.2024.1526432/full
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