Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Daniel Pastor–Galán"'
Autor:
Mingshuai Zhu, Daniel Pastor–Galán, Matthijs A. Smit, Dorjgochoo Sanchir, Fuqin Zhang, Chenghao Liu, Ye Luo, Laicheng Miao
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 10, Pp n/a-n/a (2024)
Abstract The opening of oceans within accretionary orogens is important for understanding the Wilson cycle. The Mongol–Okhotsk Ocean (MOO) began opening within the early Paleozoic accretionary collage of the Central Asian Orogenic Belt (CAOB), repr
Externí odkaz:
https://doaj.org/article/006b2f196bf748988b0497a0013c3d3f
Autor:
Suzanna van de Lagemaat, Daniel Pastor-Galán, Bas Zanderink, Maria Villareal, John Jenson, Mark Dekkers, Douwe van Hinsbergen
The kinematic history of the Philippine Sea Plate (PSP) is crucial for interpreting its geological record related to subduction initiation processes and the paleogeography of the junction between the Paleo-Pacific and Tethyan oceanic realms. However,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25b6e95891843d1ad02e38407869f206
https://doi.org/10.31223/x53m3p
https://doi.org/10.31223/x53m3p
Autor:
Mingshuai Zhu, Zhiyong Yan, Daniel Pastor-Galán, Lin Chen, Laicheng Miao, Fuqin Zhang, Shun Li, Shunhu Yang
Publikováno v:
Geology.
Subduction initiation is a pivotal process in plate tectonics. Models of subduction initiation include the collapse of passive margins, oceanic transform faults, inversion of oceanic core complexes, and ridge failure but have ignored the potential ef
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9d9bfb7cf70876f013e4c41dcde0853
https://doi.org/10.1130/g51222.1
https://doi.org/10.1130/g51222.1
Autor:
Rafael Guerra Roel, Daniel Pastor Galán, Gabriel Chávez Cabello, César Francisco Ramírez-Peña, José Jorge Aranda Gómez, Gerardo Patiño Méndez, Alejandro Rodríguez-Parra, Eduer Giovanny Nova Rodríguez, Roberto Stanley Molina Garza
The Mexican Fold-and-Trust Belt is a winding belt that formed after a series of protracted tectonic events, which began with the onset of sedimentation in the basins formed during the break-up of Pangea and during the roll-back of the oceanic Kula pl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e387f55f25a8bacc7640f8dfe4abaeaf
https://doi.org/10.5194/egusphere-egu23-324
https://doi.org/10.5194/egusphere-egu23-324
The Central Asian Orogenic Belt (CAOB) consists of several continental blocks, was assembled during the Phanerozoic, and preserves large volumes of Phanerozoic granitoids with juvenile Nd and Hf isotope characteristics, and thus regarded as the large
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7da962a90bf07dad91cc46fba39c2db4
https://doi.org/10.5194/egusphere-egu23-4201
https://doi.org/10.5194/egusphere-egu23-4201
The Tethyan oceans are the internal sotry-tellers of the amalgamation, tenure and break up of Pangea. All tethyan oceans have been mostly consumend and only remnants of them occur now along the margins of the Atlantic, Mediterranean, Black and Caspia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::930cc9401957acc9ca4634206ae99712
https://doi.org/10.5194/egusphere-egu23-3799
https://doi.org/10.5194/egusphere-egu23-3799
Autor:
Mingshuai Zhu, John Wakabayashi, Daniel Pastor-Galán, Fuqin Zhang, Ariuntsetseg Ganbat, Laicheng Miao, Shunhu Yang, Zeli Wang
Publikováno v:
GSA Bulletin.
The Late Paleozoic−Mesozoic Mongol-Okhotsk orogenic belt marks the final aggregation of East Asia. The geodynamics of the Mongol-Okhotsk oceanic plate subduction are still poorly understood due to its curved orogenic architecture, complex kinematic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::367ecaa905044e0e63880adbd92aad66
https://doi.org/10.1130/b36644.1
https://doi.org/10.1130/b36644.1
Autor:
Mingshuai Zhu, Fuqin Zhang, Matthijs A. Smit, Daniel Pastor‐Galán, Carl Guilmette, Laicheng Miao, Yi Zou, Shunhu Yang, Ariuntsetseg Ganbat, Lorraine Tual, Zeli Wang
Publikováno v:
Journal of Geophysical Research: Solid Earth. 128
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2552b982800225dade57fef3e3f94ae4
https://doi.org/10.1029/2022jb025388
https://doi.org/10.1029/2022jb025388
Autor:
Daniel Pastor-Galán, Kazumasa Aoki, Shogo Aoki, Nelson Boniface, Ariuntsetseg Ganbat, Tatsuki Tsujimori
Publikováno v:
Gondwana Research. 91:286-306
The Ubendian Belt between the Archean Tanzania Craton and the Bangweulu Block, represents a Paleoproterozoic orogeny of these two constituents of the Congo Craton assembled at ~1.8 Ga, forming the Central African Shield, during the Columbia Supercont
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4ca65e30968d8e68728e5647a778fcf
https://doi.org/10.1016/j.gr.2020.12.009
https://doi.org/10.1016/j.gr.2020.12.009
Autor:
M. Hofmann, E. Núñez-Guerrero, Alicia López-Carmona, Daniel Pastor-Galán, Juan Ramón Colmenero, Ulf Linnemann, Gabriel Gutiérrez-Alonso, A. Martínez García, Juan Carlos Gutiérrez-Marco, Javier Fernández-Suárez, Enrique Bernárdez
Publikováno v:
Geological Society, London, Special Publications. 503:563-588
The Cantabrian Zone, in the Variscan belt of Western Europe, has one of the most continuous Ediacaran–Paleozoic stratigraphic successions in the world. This succession has been extensively studied, including several detrital zircon U–Pb geochrono
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d6efa573d46597d0b1533f7d9bbb3e8
https://doi.org/10.1144/sp503-2020-21
https://doi.org/10.1144/sp503-2020-21