Results 211 to 220 of about 87,823 (291)
Some of the next articles are maybe not open access.
Earth-Science Reviews, 2018
The South China Craton consists of the Yangtze and Cathaysia blocks that were welded together along the Jiangnan Fold Belt in the Neoproterozoic. The Neoproterozoic magmatism in the western and northern margins of the Yangtze Block is characterized by ...
Junhong Zhao +3 more
semanticscholar +1 more source
The South China Craton consists of the Yangtze and Cathaysia blocks that were welded together along the Jiangnan Fold Belt in the Neoproterozoic. The Neoproterozoic magmatism in the western and northern margins of the Yangtze Block is characterized by ...
Junhong Zhao +3 more
semanticscholar +1 more source
Cretaceous volcanic-plutonic magmatism in SE China and a genetic model
, 2020Intensive and extensive Cretaceous volcanic-plutonic magmatism occurred in the coastal area of SE China, which is an important part of circle Pacific continental margin associated with copper and gold metallogenesis.
Xi‐sheng Xu +4 more
semanticscholar +1 more source
Gangdese magmatism in southern Tibet and India–Asia convergence since 120 Ma
Special Publications, 2018A compilation of 290 zircon U–Pb ages of intrusive rocks indicates that the Gangdese Batholith in southern Tibet was emplaced from c. 210 Ma to c. 10 Ma.
Di‐Cheng Zhu +4 more
semanticscholar +1 more source
Continental crust formation on early Earth controlled by intrusive magmatism
Nature, 2017Antoine B Rozel +2 more
exaly +2 more sources
, 2020
The Porto Belo Complex orthogneisses are dominantly intermediate, high-K calc-alkaline rocks of Tonian age (ca. 800 Ma) that represent the hinterland basement of northern Dom Feliciano Belt.
G. Toni +5 more
semanticscholar +1 more source
The Porto Belo Complex orthogneisses are dominantly intermediate, high-K calc-alkaline rocks of Tonian age (ca. 800 Ma) that represent the hinterland basement of northern Dom Feliciano Belt.
G. Toni +5 more
semanticscholar +1 more source
Lithos, 2019
Indentation of the Arabian platform into the eastern domain of the Anatolide-Tauride Block (ATB) led to sub-horizontal rupture and break-off of the Arabian segment of the subducting southern Neotethyan oceanic slab beneath ATB in the late Cenozoic ...
Fabien Rabayrol, C. Hart, D. Thorkelson
semanticscholar +1 more source
Indentation of the Arabian platform into the eastern domain of the Anatolide-Tauride Block (ATB) led to sub-horizontal rupture and break-off of the Arabian segment of the subducting southern Neotethyan oceanic slab beneath ATB in the late Cenozoic ...
Fabien Rabayrol, C. Hart, D. Thorkelson
semanticscholar +1 more source
The Cretaceous-Paleogene Mexican orogen: Structure, basin development, magmatism and tectonics
Earth-Science Reviews, 2017The Mexican orogen is the expression in Mexico of the Cordilleran orogenic system. The orogen extends the length of Mexico, a distance of 2000 km from the state of Sonora in the northwest to the state of Oaxaca in the south.
E. Fitz-Díaz +3 more
semanticscholar +1 more source
GSA Bulletin, 2019
Postcollisional magmatism in the eastern Sakarya zone was recorded by voluminous basic volcanism and repeated plutonism during the early Cenozoic.
Abdurrahman Dokuz, F. Aydın, O. Karslı
semanticscholar +1 more source
Postcollisional magmatism in the eastern Sakarya zone was recorded by voluminous basic volcanism and repeated plutonism during the early Cenozoic.
Abdurrahman Dokuz, F. Aydın, O. Karslı
semanticscholar +1 more source
Journal of Asian Earth Sciences, 2018
The widespread large-scale Mo-Au-Pb-Zn mineralization in the southern margin of the North China Craton (NCC) is spatially and temporally associated with the voluminous late Mesozoic granitic magmatism.
T. Zhao +5 more
semanticscholar +1 more source
The widespread large-scale Mo-Au-Pb-Zn mineralization in the southern margin of the North China Craton (NCC) is spatially and temporally associated with the voluminous late Mesozoic granitic magmatism.
T. Zhao +5 more
semanticscholar +1 more source
Tectonophysics, 2018
The origin and evolution of magmatism in rifting margins are a fundamental geological subject, and remain the focus of intense studies. Unlike the classical magma-poor and magma-rich rifting margins, the northern margin of the South China Sea (SCS ...
S. Xia +8 more
semanticscholar +1 more source
The origin and evolution of magmatism in rifting margins are a fundamental geological subject, and remain the focus of intense studies. Unlike the classical magma-poor and magma-rich rifting margins, the northern margin of the South China Sea (SCS ...
S. Xia +8 more
semanticscholar +1 more source