Results 81 to 90 of about 166,331 (170)

The geology of the Aracruz pluton (Espírito Santo, Brazil), a Cambrian post-orogenic intrusion in the aftermath of Gondwana amalgamation

open access: yesJournal of Maps
We present the first geological map of the Aracruz pluton (Espírito Santo, Brazil), which belongs to the late Cambrian post-orogenic suite that intruded the Nova Venécia metapelites and Ediacaran syn-orogenic S-type granites of the Araçuaí belt.
Andrea Galli   +12 more
doaj   +1 more source

Geology, alteration, mineralization and geochemistry at south of Arghash (Neyshabour)

open access: yesJournal of Economic Geology, 2011
The Arghash area is located 45 km to southwest of Neyshabour. The subvolcanic rocks in the area consist of biotite hornblende quartz monzodiorite porphyry, hornblende biotite quartz monzodiorite porphyry, hornblende monzonite porphyry, biotite hornblende
Zahra Karimi Saeidabadi   +2 more
doaj   +1 more source

Texture and trace element geochemistry of quartz in skarn system: perspective from Jiguanzui Cu-Au skarn deposit, Eastern China

open access: yes, 2019
The Jiguanzui Cu–Au deposit is an important skarn deposit in the Edong ore district of the Middle–Lower Yangtze River Valley Metallogenic Belt (MLYRB), Eastern China.
Tian, J (15686213)   +9 more
core   +2 more sources

Petrology, Magnetic susceptibility, Tectonic setting and mineralization associated with Plutonic and Volcanic Rocks, Eastern Bajestan and Taherabad, Iran

open access: yesJournal of Economic Geology, 2010
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

The Wiley Glacier complex, Antarctic Peninsula: pluton growth by pulsing of granitoid magmas

open access: yes, 1997
Early Cretaceous gabbro, quartz-diorite-granodiorite, and tonalite-granodiorite plutons of the Wiley Glacier complex, in the Antarctic Peninsula magmatic arc, were emplaced in a zone of syn-magmatic extensional shearing.
Vaughan, Alan P.M.   +5 more
core   +1 more source

Petrography of the Dren-Bohula massif as a part of the ophiolitic complex Demir Kapija–Gevgelija [PDF]

open access: yes, 2021
The Dren-Bohula massif covers the western parts of the ophiolite complex Demir Kapija Gevgelija and geologically it does not represent a separate tectonic segment.
Boev, Ivan
core  

Hybridization of mafic microgranular enclaves: mineral and whole-rock chemistry evidence from the Karamadazi Granitoid, Central Turkey

open access: yes, 2006
On the Eastern Tauride Belt, the Cretaceous calc-alkaline Karamadazi Granitoid consists of quartz diorite containing mafic microgranular enclaves (MME) and leucocratic granite. The quartz diorite consists of plagioclase (An(8-65)), hornblende, biotite, K-
Kocak, Kerim
core   +1 more source

Petrogenesis of Bir Madi Gabbro-Diorite and Tonalite-Granodiorite Intrusions in Southeastern Desert, Egypt: Implications for Tectono-Magmatic Processes at the Neoproterozoic Shield [PDF]

open access: yesInternational Journal of Economic and Environment Geology, 2010
The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite Complex (GDC) and a Tonalite-Granodiorite Suite (TGrS).
M. A. OBEID
doaj  

Petrogenesis and Economic Potential of the Almogholagh Intrusive Body, Using the Zircon Chemistry; Central Sanandaj-Sirjan Zone

open access: yesJournal of Economic Geology
In this study, the mineralization potential of the Almogholagh intrusive rocks (Northwest Hamedan), Central Sanandaj-Sirjan Zone, was investigated using the chemical composition of zircon grains. The Almogholagh intrusive rocks comprises three main types
Fatemeh Sarjoughian   +2 more
doaj   +1 more source

Изменение строения поверхности гетерогенного тела (диорита) при трении

open access: yes, 2018
Raman, infrared, and photoluminescent spectroscopy has been used to study changes in the surface structure of quartz diorite caused by friction. Before friction, the diorite surface layer has contained mainly quartz and feldspar crystals. After friction,
В.И. Веттегрень   +6 more
core   +1 more source

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