Results 1 to 10 of about 370 (183)
Scavenging and release of REE and HFSE by Na-metasomatism in magmatic-hydrothermal systems [PDF]
Exploitable or potentially exploitable deposits of critical metals, such as rare-earth (REE) and high-field-strength elements (HFSE), are commonly associated with alkaline or peralkaline igneous rocks.
Wu-Bin Yang +5 more
doaj +3 more sources
Reaction-driven magmatic crystallisation at the Maoniuping carbonatite [PDF]
Igneous rocks form by solidification of magmas through cooling or volatile degassing following decompression. Expelled H2O is thought to trigger alteration around intrusions, leading to formation of metasomatic halos.
Yan Liu, Michael Anenburg
doaj +2 more sources
A new occurrence of hydrous andradite within pyroclastic rocks of the Sierra De Bahoruco, Dominican Republic [PDF]
The titanium-bearing (up to 3.31 wt% TiO2) hydrous andradite [Ca2.98Na(0.02)K(0.01)Fe2+ (0.01)]Σ=3.02[Fe3 + 1.25Al0.45Ti0.15Fe2+ 0.07Mg0.04V3+ 0.01Mn2+ 0.01]Σ=2.98Si2.43O9.72(OH)2.28 was identified within intensely altered and weathered pyroclastic ...
Jacek Wachowiak +8 more
doaj +2 more sources
Different forms of talc have been developed in the first member of Permian Maokou Formation (P2m1) in the Sichuan Basin. As a hydrothermal alteration mineral, its formation mechanism and its influence on the P2m1 reservoir need to be further explored ...
Haixia REN +6 more
doaj +1 more source
At Mid‐Ocean Ridges, hot, reduced, acidic, and metal‐rich fluids are responsible for the formation of ultramafic‐hosted seafloor massive sulfide deposits (UM‐SMSs), where mantle exhumation efficiently operates.
R. Coltat +5 more
doaj +1 more source
Hiekkapohja hydrothermal system – ore mineral, lithogeochemical and paleomagnetic evidence from the Paleoproterozoic Central Finland Granitoid Complex [PDF]
The Paleoproterozoic Svecofennian Central Finland Granitoid Complex (CFGC) has been regarded as an area of low mineralisation potential. The Hiekkapohja area, 20km north-east of the town of Jyväskylä, host a concentration of variable metalliferous ...
Esa Heilimo +4 more
doaj +1 more source
Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia [PDF]
In the Risovaca cave are found, for the karst, atypical alteration in the limestones structure. Also, morphogenesis of the object can not be logically interpret. Those differences are result of hydrothermal process in initial phase of karstic cycle.
Wrzak-Tomić Janina, Manecki Andrzej
doaj +1 more source
Archean metavolcanics from the Mauranipur Structure of the Central Bundelkhand greenstone complex have been subjected to three stages of metamorphism and metasomatism: 1) amphibolite-facies metamorphism (~2.7 Ga), 2) retrograde metamorphism and ...
Олег Станиславович Сибелев +1 more
doaj +1 more source
Geochemical characteristics of the garnets from the Laodonggou gold deposit, Beishan, Inner Mongolia
The Laodonggou gold deposit is a medium-sized gold deposit discovered in the eastern section of the Beishan metallogenic belt. It resulted from the superposition of multi-phase and multi-stage metallogenesis.
TANG Weidong +8 more
doaj +1 more source
Rare Earth Elements (REE) + Niobium (Nb) + Uranium (U) + Zircon (Zr) + Lithium (Li) formations are investigated which are related with alkaline Upper Cretaceous - Lower Paleocene Kuluncak Syenitoid that settled by cutting the Kuluncak ophiolite in the ...
Okan Pulat +2 more
doaj +1 more source

