Results 91 to 100 of about 376,087 (268)
U–Pb Dating of Cambrian Magmatism in the Pinerolo‐Sanfront Unit, Dora‐Maira Massif (Western Alps)
ABSTRACT The Pinerolo‐Sanfront Unit (PSU), the structurally lowest tectonic unit of the Dora‐Maira Massif (Western Alps), has been regarded as a monocyclic unit composed of Permo‐Carboniferous sediments and Permian granitoids that were metamorphosed during the Alpine orogeny.
Francesco De Cesari +6 more
wiley +1 more source
ABSTRACT The Southern Brasília Orogen formed during Western Gondwana's final assembly and comprises nappe systems piled against the São Francisco Craton. We present new rutile U–Pb ages from the lowermost Canastra Group (> 2.2 Ga) and the uppermost Carrancas Group (~560 Ma), integrated with published zircon, monazite, garnet, and mica ages from the ...
Rodrigo Irineu Cerri +7 more
wiley +1 more source
supplementary material of "Newly recognized retrograde eclogites overprinted by high temperature metamorphism in Amdo microcontinent, Central Tibet: Implications for subduction erosion during continental subduction"THIS DATASET IS ARCHIVED AT
Peng, Y (via Mendeley Data) +1 more
core +1 more source
Tectonics of Part of the Vinodol Valley Within the Model of the Continental Crust Subduction
The Vinodol valley is analysed as an example of one of the unitedzones of shallow continental subduction. The structural analysistogether with the interpretation of structural dynamics of the centralpart of the valley is performed in that sense.
Ivan Blašković
doaj +1 more source
A numerical study of the dynamics of subduction [PDF]
The mechanics and dynamics of subduction have been studied using 2-D finite element analysis. Two finite element formulations have been employed; one formulation for Newtonian viscous flow and one formulation for linear elasticity and viscoelasticity ...
Whittaker, A.
core
Microcontinents and Continental Fragments Associated With Subduction Systems
Microcontinents and continental fragments are small pieces of continental crust that are surrounded by oceanic lithosphere. Although classically associated with passive margin formation, here we present several preserved microcontinents and continental ...
J. M. van den Broek +3 more
core +1 more source
The present continental crust is characterized by a felsic upper crust and a mafic lower crust, resulting from significant geochemical differentiation over geological time.
Long Tian +7 more
doaj +1 more source
The Mesozoic subduction zone over the Dongsha Waters (DSWs) of the South China Sea (SCS) is a part of the westward subduction of the ancient Pacific plate.
Pibo Su, Zhongquan Zhao, Kangshou Zhang
doaj +1 more source
Changing Sources of Magma Generation Beneath Intra-Oceanic Islands Arcs: An Insight From the Juvenile Kohistan Island Arc, Pakistan Himalaya [PDF]
The Kohistan arc, situated in the Pakistan Himalaya, is a Cretaceous intraoceanic island arc which was initiated during the northward movement of the Indian Plate. The arc was sutured to Asia at ca. 100 Ma.
Petford, Nick; id_orcid +4 more
core +1 more source
The physical and chemical processes that occur during the subduction of two converging tectonic plates have significant consequences, contributing to both the growth of the continental crust and the chemical and thermal evolution of the Earth's interior.
Eggins, S., Tatsumi, Y.
core

