Results 101 to 110 of about 2,212 (216)
Basic-intermediate igneous rocks formed by transformastion processes in the SW of Spain
Transformation of granitic rocks in contact with marly-carbomnate rocks to diorites gabros and peridotites is a normal situation in the Hercinyan of SpainPeer ...
Sánchez Cela, Vicente +1 more
core
Alkaline magmas in shallow arc plutonic roots: a field and experimental investigation of hydrous cumulate melting in the southern Adamello batholith. [PDF]
Pimenta Silva M +5 more
europepmc +1 more source
The paper presents new data on the composition of Late Paleozoic terrigenous and volcanogenic-terrigenous rocks of the Upper Devonian-Lower Carboniferous Tocher formation of the Bagdarin synform (Western Transbaikalia).
V. S. Tashlykov +4 more
doaj +1 more source
Mineral chemistry dataset of the Tournaisian - Lower Viséan submarine basaltic volcanism of the Matachel Basin (SW Iberian Massif). [PDF]
Sarrionandia F +5 more
europepmc +1 more source
Late Cretaceous plutonic rocks are commonly observed along the Southeastern Anatolian Orogenic Belt (SAOB), which constitutes a significant part of the Alpine–Himalayan Orogenic Belt.
Abdullah Sar, Mustafa Eren Rizeli
core +1 more source
Hercynian gabbroic, dioritic and tonalitic rocks crop out in the neighbourhood of Rovale (Sila Grande, Calabria). They make up a crude rectangular outcrop with the western part consisting of gabbroic rocks and the eastern of dioritic and tonalitic rocks.
PICCARRETA G. +2 more
core
The geochemistry, origin, and hydrothermal alteration mapping associated with the gold-bearing quartz veins at Hamash district, South Eastern Desert, Egypt. [PDF]
Abdel-Rahman AM +5 more
europepmc +1 more source
The geologic history of Vermont is marked by two significant tectonic events; the Taconian and Acadian Orogenies, dated at 460-440 and 400-360 Ma, respectively. A Siluro-Devonian dike complex of the New Hampshire sequence, north eastern Vermont, has been
Ashaki A. Rouff (1448917)
core
The Shahira Layered Mafic Intrusion (SLMI), which belongs to the late Neoproterozoic plutonic rocks of the Arabian-Nubian Shield, is the largest layered mafic intrusion in southern Sinai.
M.K. AZER, M.A. OBEID, H.A. GAHLAN
doaj

