نتایج جستجو برای: hydrothermal alteration mapping

تعداد نتایج: 258863  

Calagari, AliAsghar, Miranvari, Azam Sadat, Siahcheshm, Kamal, Sohrabi, Ghahraman,

The Zailic gold-bearing veins are located in the Arasbaran metallogenic zone, east of Ahar, East-Azarbaidjan Province. The most important lithologic units in this area are andesitic and trachy-andesitic tuffs and lavas of Upper Eocene age hosting vein-type gold mineralization. Theses rocks have suffered silicic, argillic, phyllic, and propylitic alterations brought about by hydrothermal fluids....

Baharifar, , Khodaean Chegeni, , Maria Conte, , Rashidnejad Omran, , Vaccaro, ,

The garnet calc-silicates at Baba-Nazar are located in the NE of Takab, Sanandaj- Sirjan zone. Anhedral to euhedral green colored garnets is a characteristic feature of these Calc-silicates. Mineral chemistry shows that garnets are Andradite- Grossular and contain more than 13% uvarovite. The high chromium content garnet, Cr-Spinel that have relatively Cr rich core than the rim, sulfide opaque ...

2008
R. V. Morris G. Klingelhöfer C. Schröder I. Fleischer D. W. Ming A. S. Yen R. Gellert R. E. Arvidson D. S. Rodionov L. S. Crumpler B. C. Clark B. A. Cohen T. J. McCoy D. W. Mittlefehldt M. E. Schmidt P. A. de Souza S. W. Squyres

[1] Spirit’s Mössbauer (MB) instrument determined the Fe mineralogy and oxidation state of 71 rocks and 43 soils during its exploration of the Gusev plains and the Columbia Hills (West Spur, Husband Hill, Haskin Ridge, northern Inner Basin, and Home Plate) on Mars. The plains are predominantly float rocks and soil derived from olivine basalts. Outcrops at West Spur and on Husband Hill have expe...

2008
R. V. Morris G. Klingelhöfer C. Schröder I. Fleischer D. W. Ming A. S. Yen R. Gellert R. E. Arvidson D. S. Rodionov L. S. Crumpler B. C. Clark B. A. Cohen T. J. McCoy D. W. Mittlefehldt M. E. Schmidt P. A. de Souza S. W. Squyres

[1] Spirit’s Mössbauer (MB) instrument determined the Fe mineralogy and oxidation state of 71 rocks and 43 soils during its exploration of the Gusev plains and the Columbia Hills (West Spur, Husband Hill, Haskin Ridge, northern Inner Basin, and Home Plate) on Mars. The plains are predominantly float rocks and soil derived from olivine basalts. Outcrops at West Spur and on Husband Hill have expe...

2006
Christine Laverne Olivier Grauby Jeffrey C. Alt Marcel Bohn

[1] Hydroschorlomite, a Ti-, Ca-, Fe-rich andraditic garnet present in the deepest cores of basalts (661– 749 mbsf) drilled in Hole 1256D during Ocean Drilling Program (ODP) Leg 206 (equatorial east Pacific), is reported here for the first time in oceanic crust. Detailed petrological and mineralogical studies by optical microscope, electron microprobe, scanning and transmission electron microsc...

نریمانی, فاطمه, بدیعی, علیرضا, خرامش, محمد , طوطی, فرامرز,

Hydroxy davyne is a hydrated aluminosilicates with the same structure as cancrinite mineral group. Scientist categorized hydroxy davyne as zeolite because of its low temperature formation conditions and hydrated structure. Existence of [Ca.Cl] + group instead of [Na.H2O] + group is the significant property of this mineral. Alteration of volcanic ash in presence of alkaline hydrothermal solution...

2011
S. P. Schwenzer

Home Plate is a plateau in the Columbia Hills of Gusev Crater [1]. It is a layered sequence of clastic rocks with alkali basaltic composition. Based on stratigraphy, structure, sedimentology, mineralogy, and bulk chemistry it is interpreted as pyroclastic deposit and thought to be extensively hydrothermally altered [1-5]. The hydrothermal alteration is presumed to be of high and low temperature...

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