Results 111 to 120 of about 806 (206)
Eocene intermediate to felsic plutons of different sizes and compositions are widespread in the Eastern Pontides Orogenic Belt in northern Turkey. Of these, the Taşlık Tepe pluton in the Havza (Samsun) area is fine-to-medium-grained, with granular ...
Mehmet Arslan (593290) +5 more
core +1 more source
Archean continental crust formed by magma hybridization and voluminous partial melting. [PDF]
Hernández-Montenegro JD +3 more
europepmc +1 more source
Arghash – Ghasem-Abad area in NE Iran is located in the rim of the Sabzevar structural zone. Tertiary outcrops include granite and quartz monzodiorite porphyry associated with dacite and andesite volcanic rocks.
Zahra Alaminia +3 more
doaj
The Sendai river terraces monitored the co-seismic mega-thrusting. [PDF]
Osozawa S, Ito H.
europepmc +1 more source
Understanding the petrogenesis of Miocene adakite-like igneous rocks is crucial for unraveling the formation processes of post-collision porphyry copper deposits within the Gangdese orogenic belt. This study focuses on the mineralogical, geochronological,
Zhao, Jiaxuan +5 more
core +1 more source
A new concept for the genesis of felsic magma: the separation of slab-derived supercritical liquid. [PDF]
Taniuchi H +4 more
europepmc +1 more source
The petrogenesis and geodynamic setting of the Mesozoic magmatic rocks in the Erguna Block, NE China remains controversial, especially the relationship between magmatism and the subduction history of the Mongol–Okhotsk oceanic plate.
Yuanchao Wang +3 more
core +1 more source
Hypogene enrichment in Miduk porphyry copper ore deposit, Iran. [PDF]
Yousefi Soorani L +4 more
europepmc +1 more source
Macedonian Eastern Vardar Ophiolitic unit represents a part of the Neotethys that was obducted onto the European Margin (Serbian Macedonian Massif). It comprises of well exposed sheeted dykes complex, with pillow lavas as a top unit, which is intruded by
Romer, Rolf +5 more
core +1 more source
The granodiorite intrusions with associated Cu-Au skarn mineralization of La Paz district are located in the east part of the Mesa Central of Mexico. The skarn developed at the contact between a middle Cretaceous calc-argillaceous sedimentary sequence ...
Porfirio J. Pinto-Linares +6 more
doaj

