Results 21 to 30 of about 3,139 (203)

Geochemistry, Geochronology and mineralisation potential of the granites in the Central Iberian Zone: The Jalama batholith [PDF]

open access: yes, 2008
The Jalama batholith (Spain and Portugal) is one of the numerous granites ofthe Central Iberian Zone with Sn- and W-associated mineralisation.
Ruíz García, Casilda
core   +2 more sources

Interaction of B-rich supercritical magmatic fluids with granite: first report of dumortierite in Larderello, Italy [PDF]

open access: yesE3S Web of Conferences, 2019
In a peraluminous two-mica monzogranite cored at 4.5 km depth in well Radicondoli 29, dumortierite occurs together with andalusite, Li-rich tourmaline, fluorite and fluorapatite.
Puxeddu Mariano
doaj   +1 more source

Evidence for present-day leucogranite pluton growth in Tibet [PDF]

open access: yesGeology, 2004
Several geophysical surveys carried out in southern Tibet have revealed the occurrences of bright spots of high electrical conductivity at 15–20 km depth, corresponding to zones of seismic attenuation and correlated to high heat flow at the surface.
Gaillard, Fabrice   +2 more
openaire   +1 more source

Le magmatisme de la région de Kwyjibo, Province\ud du Grenville (Canada) : intérêt pour les\ud minéralisations de type fer-oxydes associées [PDF]

open access: yes, 2005
The granitic plutons located north of the Kwyjibo property in Quebec’s Grenville Province are of\ud Mesoproterozoic age and belong to the granitic Canatiche Complex . The rocks in these plutons are calc-alkalic, K-rich,\ud and meta- to peraluminous. They
Bain J.H.C.   +40 more
core   +3 more sources

On the geodynamics of the Alpine collisional granitoids from Central Anatolia: petrology, age and isotopic characteristics of the granitoids of the Ekecikdağ Igneous Association (Aksaray/Turkey)

open access: yesGeodinamica Acta, 2019
Granitoids of the Ekecikdağ Igneous Association (Central Anatolia/Turkey) are products of collisional–post-collisional magmatism in the Ekecikdağ area. These granitoids are granodiorite, microgranite and leucogranite.
Fatma Toksoy-Köksal
doaj   +1 more source

Mapping of Himalaya Leucogranites Based on ASTER and Sentinel-2A Datasets Using a Hybrid Method of Metric Learning and Random Forest

open access: yesIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 2020
The widely distributed leucogranite belt in the Himalayan orogeny is expected to have excellent potential for developing rare metal mineralization.
Ziye Wang, Renguang Zuo, Yanni Dong
doaj   +1 more source

Chemical diffusivity of boron in melts of haplogranitic composition [PDF]

open access: yes, 1993
Chemical diffusivities of B in synthetic melts of haplogranitic composition have been measured by the diffusion couple technique at 1 atm between 1200–1600°C.
Chakraborty, Sumit   +2 more
core   +1 more source

Granite magmatism and mantle filiation [PDF]

open access: yesEuropean Journal of Mineralogy
Current granite magma generation models essentially reduce to two groups: (1) intra-crustal melting and (2) basaltic origin. A mixed, crustal, and basaltic origin and therefore a mantle filiation has been proposed for most granite magma types.
M. Pichavant   +3 more
doaj   +1 more source

The Encantada Granite: registration of a peraluminous intrusion in the Rondonian Province - San Ignacio, in SW Amazonic Craton, Mato Grosso, Brazil [PDF]

open access: yesGeologia USP. Série Científica, 2015
The Encantada Granite occurs on the extreme southwest of the state of Mato Grosso, SW of the Amazonian Craton, near the border of Brasil/Bolívia. It corresponds to an body oriented to NNW direction that intruded metasedimentary and metavolcanic rocks ...
Brena Verginassi do Nascimento   +2 more
doaj   +1 more source

Structure of late Variscan Millevaches leucogranite massif in the French Massif Central: AMS and gravity modelling results [PDF]

open access: yes, 2006
In the Limousin area, Variscan leucogranitic plutons are spatially associated with normal faults and major strike-slip shear zones that are a continuation of the South Armorican shear zone. Our study focuses on the large N-S-trending Millevaches granitic
Arthaud   +46 more
core   +4 more sources

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