Results 61 to 70 of about 21,455 (215)

Riphean magmatism and ore formation, preceding the disclosure of the Uralian Paleoocean (western slope of the Southern Urals)

Литосфера, 2017
The analysis of the evolution of composition and mineral occurences of the Low and Middle Riphean magma-tic rocks from the riftogenic structures of the Bashkirian anticlinorium involving of some neighboring structures from the western slope of the ...
V. V. Holodnov, G. B. Fershtater, E. S. Shagalov, G. Yu. Shardakova   +3 more
doaj   +2 more sources

Two episodes of Late Paleozoic A-type magmatism in the Qunjisayi area, western Tianshan: Petrogenesis and tectonic implications

, 2015
A-type magmatism is an effective lithoprobe for constraining the tectonic evolution of orogenic belts. In this study, we have identified two episodes of Late Paleozoic A-type magmatism in Qunjisayi, western Tianshan. Zircon U-Pb geochronology has yielded
Shan, Qiang, Yang, Wu-Bin, Li, Ning-Bo, Niu, He-Cai   +3 more
core   +1 more source

Linking magmatism with collision in an accretionary orogen [PDF]

, 2016
A compilation of U-Pb age, geochemical and isotopic data for granitoid plutons in the southern Central Asian Orogenic Belt (CAOB), enables evaluation of the interaction between magmatism and orogenesis in the context of Paleo-Asian oceanic closure and ...
Li, S., Guo, Q., Wang, T., Xiao, W., Chung, S., Wilde, Simon   +5 more
core   +1 more source

Neogene-Quaternary magmatic activity and its geodynamic implications in the Central Mediterranean region

Annals of Geophysics, 1997
The petrogenesis and time/space distribution of the magmatism associated with the formation of the Northern and Southern Tyrrhenian basins, together with the directions and ages of lithospheric extension and/or spreading north and south of the 410N ...
G. Serri
doaj   +1 more source

Flux Modulated Magmatic Architecture in Continental Magmatic Arcs

Petrochronology of the magmatic reservoir that underpinned the Chaxas Volcanic Complex for the duration of its 8.59 – 1.24 Ma lifecycle reveals that magmatic architecture can be regulated by magmatic flux. Modulation of the magmatic reservoir was controlled via two distinct flux regimes during the Pre-Chaxas and Chaxas Complex stages of the Chaxas ...
Charles Lewis, Shan de Silva
openaire   +1 more source

Intermontane basins and bimodal volcanism at the onset of the Sveconorwegian Orogeny, southern Norway

, 2014
This research was supported by the University of St Andrews and the Natural Environment Research Council Steering Committee (IMF458/0512 and IP-1326-0512).The greenschist-facies late Mesoproterozoic Bandak succession in southern Norway consists of ...
Roberts, Nick M.W., Roberts, N., Spencer, Christopher, Prave, Anthony R., Horstwood, Matthew S.A., Hawkesworth, C., Cawood, Peter A., Antonini, Afra S.M., Prave, A., Antonini, A., Hawkesworth, Chris J., Cawood, P., Horstwood, M., Spencer, Christopher J.   +13 more
core   +1 more source

Magmatism of Shatsky Rise controlled by plume-ridge interaction

, 2023
Data of the manuscript titled Magmatism of Shatsky Rise controlled by plume-ridge ...
Xiyuan Bao (14619217), Eric L. Brown (14619210), Jinchang Zhang (14619213), Xubo Zhang (14619207), Jian Lin (14619216), William W. Sager (14619219)   +5 more
core   +1 more source

The Contentnea Creek Granite : Constraints On Late Paleozoic Magmatism And Deformation, Eastern Piedmont Fault System, North Carolina

, 2023
The Alleghanian orogeny is manifested in eastern North Carolina by dextral transpressional faulting on the Eastern Piedmont Fault system and spatially associated granitic magmatism.
Burns, Richard W., NC DOCKS at East Carolina University   +1 more
core  

Subduction zone magmatism

, 1995
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  

The plume-dependent granite-rhyolite magmatism

, 2018
The plume-dependent magmatism is widespread and well justified. The bulk of it is represented by flood basalts, basalts of oceanic islands (OIB), and basalts of oceanic plateaus (OPB), though the whole scope of plume magmatism is very diverse.
Viktor N. Puchkov
core   +2 more sources