Results 11 to 20 of about 5,193 (216)

Campiglia Marittima Skarn (Tuscany): A Challenging Example for the Evolution of Skarn-Forming Models [PDF]

open access: yesMinerals, 2023
Campiglia Marittima (hereafter Campiglia) has a long record of attracting interest on its ore deposits that have been intermittently exploited from the Copper Age to the late XX century. Since the XIX century, Campiglia has been a key locality for the debate on skarn-forming processes due to the presence of mining activities ensuring access to ever new
Vezzoni S, Rocchi S, Dini A
openaire   +3 more sources

WMo-Skarn From the Mraconia Valley, Romania [PDF]

open access: yes, 2011
International audienceThe skarn from the Mraconia was formed at the contact between crystalline limestone of the Neamtu Series and a porphyritic ranodiorite. The main metallic minerals in the Mraconia Valley are scheelite and molybdenite.
Dumitras, Delia-Georgita   +3 more
core   +7 more sources

Major and trace element analysis of common skarn minerals from Långban, Värmland, Sweden [PDF]

open access: yes, 2022
The area of Långban, Värmland, is well investigated in terms of the many exotic minerals occurring in the area. In contrast, less focus has been given to the trace element systematics of the commonly occurring skarn-forming minerals. The composition of
Persson, Lovisa
core  

Petrogenesis of skarn related Cu-porphyry intrusion deposit, Ali-Abad- Darreh Zereshk, Yazd

open access: yesJournal of Economic Geology, 2011
The study area is a part of Cenozoic magmatic belt of Central Iran, which is located in the West of Yazd porovince. Contact metamorphism and skarn occurred in conglomerate part of Sngestan Formation.
Batoul Taghipour   +1 more
doaj   +1 more source

Studies of petrography, metasomatic alteration, and genesis of Kamtal iron-copper skarn, northeast of Kharvana, East-Azarbaijan

open access: yesJournal of Economic Geology, 2012
Kamtal skarn is located 15 km northeast of Kharvana, East-Azarbaijan. A quartz-monzonitic stock of Oligocene age intruded the upper Cretaceous sedimentary sequence (claystone, limestone, marl, and siltstone) developing noticeable metamorphic (marble ...
Rasool Ferdowsi   +3 more
doaj   +3 more sources

Some mineralogical and geochemical aspects of chromium-bearing skarn minerals from northern Karelia, Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1986
The chromiferous skarn mineral associations at Outokumpu have been described and a number of characteristic chromium-bearing minerals have been re-examined.
O. von Knorring, E. Condliffe, Y.L. Tong
doaj   +1 more source

Mineralogy and Genesis of Joveinan Iron Skarn (Cenozoic Magmatic Arc, North of Isfahan) [PDF]

open access: yesپترولوژی, 2017
Joveinan marbles and skarns are located 5 km NE of Ghohrood and 140 km NW ofIsfahan in the *central part of Urumieh- Dokhtar magmatic arc. Intrusion of Ghohroodgranitoid into the Cretaceous carbonate rocks caused the contact metamorphism andformation of ...
Shahzad Sherafat   +1 more
doaj   +1 more source

Skarn garnets of the Novonikolaevskoe copper deposit (South Urals) [PDF]

open access: yesМинералогия
The paper describes the composition of skarn garnets of the Novonikolaevskoe Cu deposit (South Urals) in comparison with that of garnets of the Gumeshki and Tarutino skarn copper porphyry deposits in the Urals.
V.V. Khrebtievsky, O.Yu. Plotinskaya
doaj   +1 more source

The perigranitic W-Au Salau deposit (Pyrenees, France): polyphase genesis of a late Variscan intrusion related deposit

open access: yesBSGF - Earth Sciences Bulletin, 2021
A field study combined with a laboratory study and 3D modeling have been performed in order to decipher the genesis of the Salau deposit W-Au mineralization (Pyrenees, France), one of the most important for tungsten in Europe.
Poitrenaud Thomas   +3 more
doaj   +1 more source

KOZBUDAKLAR W-SKARN YATAĞININ JEOKİMYASAL KARAKTERİSTİKLERİ VE NADİR TOPRAK ELEMENTLERİNİN DAĞILIMLARI (BURSA, BATI ANADOLU)

open access: yesBulletin of the Mineral Research and Exploration, 2017
Kozbudaklar W-skarn yatağı Tavşanlı Zonunda Eosen Topuk granitoyidi ile Triyas İnönü mermeri arasındaki dokanakta gelişmiştir. Bölgede endoskarn zonu plajiyoklaz-piroksen, ekzoskarn zonu ise piroksen, piroksen-granat, granat ve granat-piroksen skarn ...
Ayşe ORHAN, Halim MUTLU
doaj   +1 more source

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