Results 51 to 60 of about 1,650 (203)
Study area is located in district of Bajestan and Ferdows cities, NE of Iran. Structurally, this area is part of Lut block. The oldest exposed rocks, to the north of intrusive rocks and in Eastern Bajestan, are meta-chert, slate, quartzite, thin-bedded ...
Maliheh Ghoorchi Rooki +2 more
doaj +1 more source
Granitoid magmatism along the western Pacific margin records interactions between subduction dynamics and crust–mantle processes; however, the links between plate reorganization and magma‐source evolution remain debated.
Nghiem V. Dao +7 more
doaj +1 more source
Detailed biostratigraphic study of mid-Cretaceous Tethys Himalayan pelagic units shed new light on the evolution of the northern India passive continental margin.
ISABELLA PREMOLI SILVA +2 more
doaj +1 more source
The Huangshadong geothermal field (HGF), situated in the contact zone between Mesozoic granites and NE-striking dominant faults in South China, has great geothermal potential.
Yuzhong Liao +15 more
doaj +1 more source
Evolution of the Shimanto accretionary complex suggests implications for the geological history of the East Asian continental margin. To better understand the tectonic evolution of the complex during Paleocene to early Miocene, we collected new ...
Hidetoshi Hara +2 more
doaj +1 more source
Time scale for the development of thickened crust in the Cretaceous North Cascades magmatic arc, Washington, and relationship to Cretaceous flare-up magmatism [PDF]
Erin K. Shea +7 more
openaire +1 more source
The Troiseck-Floning and Rosskogel nappes are part of the Austroalpine Unit in the eastern part of the Eastern Alps. The nappes are in tectonic contact and comprise Permian to Mesozoic lower greenschist facies metamorphic metasediments, but only the ...
Martin K. Reiser +4 more
doaj +1 more source
Late Cretaceous Magmatism in the Chelopech region, Central Srednogorie magmatic zone
Stanislav Stoykov +3 more
openaire +1 more source
Spatiotemporal Variation of the Cretaceous‐Eocene Arc Magmatism in Lhasa‐Tengchong Terrane
It was recognized that two magmatic belts in the Lhasa‐Tengchong terrane formed due to the Mesozoic‐Cenozoic Tethyan evolution. Still, their spatiotemporal variations of magmatic flare‐ups/lulls are rarely discussed.
Yongmin Liu +5 more
doaj +1 more source
SUBDUCTION RELATED MAGMATISM OF THE SOUTHERN CRIMEA: OFFSHORE AND ONSHORE
A geochemical comparison of igneous rocks of two regions of Mesozoic subduction related magmatism located on the opposite sides from the southern end of modern Crimea was carried out.
K.Ye. Shniukova
doaj +1 more source

