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Earth-Science Reviews, 2022
Continental-arc igneous rock compositions change in response to the transition from subduction to collision and these changes can reveal how the crust, lithosphere and magma sources evolved. Neotethys-related Late Cretaceous to Pleistocene subduction-and
H. S. Moghadam +9 more
semanticscholar +1 more source
Continental-arc igneous rock compositions change in response to the transition from subduction to collision and these changes can reveal how the crust, lithosphere and magma sources evolved. Neotethys-related Late Cretaceous to Pleistocene subduction-and
H. S. Moghadam +9 more
semanticscholar +1 more source
Earth-Science Reviews, 2021
A widespread project database for Devonian–Carboniferous magmatism in the Sierras Pampeanas and Frontal Cordillera between 27° and 35°S (including petrological, geochemical, geochronological, and isotope data) is reviewed along with compiled data from ...
J. Dahlquist +8 more
semanticscholar +1 more source
A widespread project database for Devonian–Carboniferous magmatism in the Sierras Pampeanas and Frontal Cordillera between 27° and 35°S (including petrological, geochemical, geochronological, and isotope data) is reviewed along with compiled data from ...
J. Dahlquist +8 more
semanticscholar +1 more source
Journal of Geophysical Research: Solid Earth, 2021
Understanding the tectonic setting in which ophiolites form is necessary to determine how they can be used to study ocean spreading and subduction zone processes.
M. Rioux +6 more
semanticscholar +1 more source
Understanding the tectonic setting in which ophiolites form is necessary to determine how they can be used to study ocean spreading and subduction zone processes.
M. Rioux +6 more
semanticscholar +1 more source
Chemical geodynamics of mafic magmatism above subduction zones
, 2020The geochemical signatures of subducting crust have been identified in various types of mafic igneous rocks at convergent plate boundaries, where island arc basalts (IAB) and continental arc andesite are accepted as the typical products of subduction ...
Yong‐Fei Zheng +4 more
semanticscholar +1 more source
Reviews in Mineralogy and Geochemistry, 2004
Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude "... the only possibility is, that epidote is a primary mineral in our tonalite, crystallizing early from the magma, i.e., before (in part also contemporaneous with) biotite ...
M. W. Schmidt, S. Poli
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Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude "... the only possibility is, that epidote is a primary mineral in our tonalite, crystallizing early from the magma, i.e., before (in part also contemporaneous with) biotite ...
M. W. Schmidt, S. Poli
openaire +5 more sources
The Cenozoic magmatism of East-Africa: Part I — Flood basalts and pulsed magmatism
Lithos, 2017 Tyrone O Rooney
exaly +2 more sources
Late Oligocene–early Miocene transformation of postcollisional magmatism in Tibet
Geology, 2019Uplift of the Tibetan Plateau is thought to be one of the most important orogenic and climate forcing events of the Cenozoic Era, associated with geodynamic changes related to India-Asia collision and subsequent continental lithosphere subduction ...
Zhengfu Guo, M. Wilson
semanticscholar +1 more source
Spatial and temporal radiogenic isotopic trends of magmatism in Cordilleran orogens
Gondwana Research, 2017 James B Chapman +2 more
exaly +2 more sources