Results 1 to 10 of about 4,197 (167)
High Mg# of the continental crust explained by calc-alkaline differentiation. [PDF]
ABSTRACTWe used compiled geochemical data to investigate the mechanisms that control Mg# (molar ratio of Mg/(Mg + FeT)) in andesitic arc lavas. We find that andesites from mature continental arcs with crustal thickness of >45 km have systematically higher Mg# than those from oceanic arcs with crustal thickness of <30 km.
Tang M, Liu X, Chen K.
europepmc +3 more sources
Radiological risk assessment and geochemical signatures of calc-alkaline bostonite dikes [PDF]
The bostonite dikes in the studied area of Egypt are one of the most radioactive felsic intrusions found in the South Eastern Desert due to their elevated levels of natural occurring radionuclides and the radiological hazards associated with them.
Ahmed E. Abdel Gawad +2 more
doaj +2 more sources
Magmatic sulfides in high-potassium calc-alkaline to shoshonitic and alkaline rocks [PDF]
We investigate the occurrence and chemistry of magmatic sulfides and their chalcophile metal cargo behaviour during the evolution of compositionally different magmas from diverse geodynamic settings both in mineralised and barren systems.
A. A. Georgatou, M. Chiaradia
doaj +1 more source
Petrography, geochemistry and petrogenesis of high-silica Adakitic rocks from Bayram Abad area in the northwest Neyshabour (Northeast of Iran) [PDF]
The volcanic rocks of Bayram Abad area, located 12 km northwest of Neyshabour, are dominated by the Paleogene units composing of dacite and andesite rocks.
mohammad ebrahim fazel valipour
doaj +1 more source
In Pagondas and Kimi areas, central Evia Island, Greece, variably serpentinized ultramafic rocks of an ophiolitic origin are crosscut by rodingite dikes.
Christos Karkalis +4 more
doaj +1 more source
In the Mississippian Matachel small volcanic field of the Ossa‐Morena Zone (southern Iberian Massif) outpoured basic‐intermediate lavas exhibit geochemical characteristics of Low‐Ti continental tholeiites and calc‐alkaline lavas.
F. Sarrionandia +5 more
doaj +1 more source
Geology, petrography, alteration, and geochemistry of the Shahrab igneous rock, Central Iran
Eocene to Quaternary calc-alkaline volcanic and intrusive rocks are exposed in Shahrab area in the Urumieh-Dokhtar magmatic belt in the Central Iran structural zone.
Kaveh Pazand +2 more
doaj +1 more source
Volcanism that has been active since the early Miocene along a N-S trending line from Eskişehir to Isparta displays calc-alkaline and alkaline character and is closely associated with slab tearing processes.
Selin Bi̇lgi̇ç Gençer +2 more
doaj +1 more source
Study of origin and petrogenesis of granitoid bodies of Soursat complex (Northwest of Takab): Whole- rock geochemical and Sr-Nd isotopic evidences [PDF]
The plutonic bodies in the Soursat complex are parts of the widespread plutonic bodies in the Sanandaj- Sirjan zone. Based on field observations and microscopic studies, the study area is dominated by hornblende gabbro, quartz diorite, monzodiorite ...
Soraya Dadfar +3 more
doaj +1 more source
The unique speciation of iron in calc-alkaline obsidians
Abstract Obsidians found in silicic domes and rhyolitic tuffs are an ideal system to understand the formation conditions of calc-alkaline felsic magmas. The Optical Absorption and Electron Paramagnetic Resonance (EPR) spectroscopic data presented in this study demonstrate that Fe-speciation in obsidians is different from that observed in other ...
Galoisy, Laurence, Calas, Georges
openaire +2 more sources

