Zobrazeno 1 - 10
of 5 404
pro vyhledávání: '"mélange"'
Publikováno v:
Open Geosciences, Vol 16, Iss 1, Pp 765-76 (2024)
The Mélange in Lamphun Province, situated in the southern region of the Chiang Mai-Chiang Rai Suture Zone (CMCRSZ), remains inadequately explored. This study employs field investigations and petrographic analysis to delineate the characteristics of
Externí odkaz:
https://doaj.org/article/d2b0cd917aa4426ea45aeab7e38c50f2
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
IntroductionArc-continent collision contributes to the accretion of continental crust in the Central Asian Orogenic Belt. The Chegendalai ophiolitic mélange, located between the Bainaimiao arc and the North China Craton, is important to understandin
Externí odkaz:
https://doaj.org/article/fd96aebb4b824b9692482a23246676bb
Publikováno v:
Progress in Earth and Planetary Science, Vol 11, Iss 1, Pp 1-17 (2024)
Abstract Lithologic heterogeneity and the presence of fluids have been linked to seamount subduction and collocated with slow earthquakes. However, the deformation mechanisms and fluid conditions associated with seamount subduction remain poorly unde
Externí odkaz:
https://doaj.org/article/28ebb8b6987b48b19a160f4349f3ef6c
Akademický článek
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Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 35, Iss 1, Pp 1-18 (2024)
Abstract On September 17th and 18th, 2022, shallow earthquakes with magnitudes of 6.6 (ML) and 6.8 (ML) occurred in the eastern Taiwan Longitudinal Valley, which marks the collision zone between the Philippine Sea plate and the Eurasian plate, and le
Externí odkaz:
https://doaj.org/article/a0e6fd7f19bf41f8947a571b7d1b1235
Publikováno v:
Геодинамика и тектонофизика, Vol 15, Iss 3 (2024)
The Alambay ophiolite zone (AOZ) is located in the axial part of the Early Paleozoic Salair orogen and includes the northern extension of the Alambay-Kaim zone, Salair and Altai Mountains. The Shalap area of the AOZ is predominantly composed of clast
Externí odkaz:
https://doaj.org/article/34200305537d48aba819225bbf920720
Publikováno v:
Геодинамика и тектонофизика, Vol 15, Iss 3 (2024)
The western margin of Central Iran – the Nain area – is composed of the Mesozoic ophiolitic mélanges deposited during the Late Cretaceous. The Nain and Darrech Deh faults whose trace indicators can be seen in the study area are among the larges
Externí odkaz:
https://doaj.org/article/9302e60efec84896b95bcf65df04b511
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 6, Pp n/a-n/a (2024)
Abstract Tectonic mélanges, characterized by conditions reflective of modern subduction fault zones, preserve mineral veins formed through mass transfer, a mechanism influencing the slip behavior of subduction megathrusts. In this study, we apply se
Externí odkaz:
https://doaj.org/article/28d881bd007842a683a9b4df858ee6aa
Publikováno v:
Earth and Space Science, Vol 11, Iss 6, Pp n/a-n/a (2024)
Abstract The Devonian tectonic setting is still controversial in the Proto‒Tethyan North Qilian belt. The Hexi Corridor of the North Qilian belt occupies a key position in constraining the tectonic evolution of the Proto‒Tethyan Ocean and the gro
Externí odkaz:
https://doaj.org/article/e1935732b3d74a2295a91d1d0bcb0f87
Publikováno v:
Геофизический журнал, Vol 45, Iss 6 (2023)
Mélange is characterized by the block-in-matrix fabric in which rigid blocks of different sizes, lithologies, and ages are distributed in a ductile matrix. Though mélange is a significant component of orogenic belts, in the Ukrainian Carpathians, m
Externí odkaz:
https://doaj.org/article/82809e376f964580a889bc76ee701541