Results 101 to 110 of about 8,056 (240)
Granitoids commonly include K-feldspar, biotite and zircon, apatite, titanite, allanite, and xenotime crystals, which are known to contain common radioactive elements.
Boztosun, Ismail +3 more
core +1 more source
The presented research is carried out in continuation of the works connected with studying the nature of radioactivity of drainage waters of quarries of Novosibirsk region, performed by the Laboratory of Hydrogeology of Sedimentary Basins of Siberia ...
Vasiliy P. Sukhorukov +3 more
doaj +1 more source
Abstract Groundwater flow regulated by deep faults remains challenging to trace due to structural complexity. This study applies the noble gas tracer 222Rn combined with hydrochemistry and stable isotopes (δ2H, δ18O) to distinguish circulation patterns of geothermal springs along a major fault in the Tibetan Plateau.
Xiaoyan Shi +7 more
wiley +1 more source
Geochronology of Portuguese granitoids: a contribution [PDF]
Geochronological data (Rb-Sr method, \87Rb = 1.42 x 10"n/y) relative to eight granitoid bodies, of which five form part of a zoned pluton (Castro Daire area, Northern Portugal), show this pluton as a multi-pulse intrusion and define four age groups (ca ...
Serrano Pinto, M.
core
U–Pb geochronology of Variscan granitoid rocks from the West Asturian Leonese Zone of the NW Iberian belt documents the episodic nature of magmatism in this section of the western European Variscides.
Jenner, G.A. +3 more
core +1 more source
The Archaean (4.0–2.5 Ga) continental crust is mainly composed of granitoids, whose geochemical characteristics are a function of their formation mechanisms and components, as well as physical conditions of their source.
Jaana Halla
doaj +1 more source
Zircon in granitoids from Sinai, Egypt and its genetic significance [PDF]
The granitic plutonism in the area around Wadi El-Sheikh, southwestern Sinai, Egypt is mainly represented by the Older and Younger Granitoid Rocks.
Salem Abdel-Karim Ahmed +2 more
core
Sumatran granitoids and their relationship to southeast Asian terranes
Three subparallel, N-S-trending granitoid provinces occur in Southeast Asia: the Eastern Granitoid Province of peninsular Malaysia; the Central Granitoid Province, extending from northwestern Thailand to the western part of peninsular Malaysia and to the
Gasparon, M (15476894) +1 more
core
Four genectic types of granitoids, i. e. mantle-derived type (M-type), syntexis type (SY-type), trasformation type [T-type, including migmatic (MT), peraluminous (PT) and K-rich (KT) subtypes], and A-type were classified in the Hercynian granitoids in ...
Bao, JX +4 more
core
Types and genesis of the enclaves in Central Anatolian granitoids
Central Anatolian granitoids range from tonalite-monzonite, through granodiorite, to alkali feldspar granite in composition, and typically have angular to oval-shaped mafic magmatic and metamorphic enclaves.
Güleç, Nilgün Türkan +2 more
core +1 more source

