نتایج جستجو برای: ophiolitic
تعداد نتایج: 353 فیلتر نتایج به سال:
Olivine is one of the major crystals in ultrabasic rocks of Piranshahr Ophiolitic Complex. This mineral occurs as anhedral with cracks and fractures. Commonly, olivine is altered to serpentine along the fractures and rims. In some cases, serpentine crosscut the olivine. According to BSE images and mineral chemistry studies of olivine, the secondary iron- rich olivines occur at the rim of primar...
The Kermanshah Ophiolite Complex (KOC) lies in the structural – tectonic zone of western Iran in northern part of Zagros main thrust and is a part of highly dismembered Kermanshah – Panjvin Ophiolitic belt. The best outcrops of the sheeted and isolated dykes in this complex are present in south of Sahneh area. They are basic in composition. The geochemical studies show parent magma is in its in...
Kamar Tallar mineralization zone in Gazik area is engulfed within ophiolitic melange in Sistan suture zone in east of Iran .The Mn- bearing ore bodies of Kamar Tallar are occurred as discontinuous patches intimately associated with cherts and meta – spilites. Field evidences and study of trenches show that the Mn- bearing patches are principally superficial and laterally limited. Braunite, Bix...
The exposed volcanic rocks in south west of the Khoy area consist of basalts with minor amounts of plagioclase-phyric basalts. These rocks are composed of clinopyroxene plus plagioclase and plagioclase phenocrysts, respectively. The basaltic rocks are highly altered and contains high amounts of secondary minerals mainly chlorite and epidote. According to mineral chemistry, the composition of cl...
In the Tethyan realm, leucocratic rocks were recognized as dikes and layers outcropping in ophiolitic of Western Alps, Corsica, Northern Apennines. Several authors have suggested that origin is associated with partial melting cumulate gabbro. Major trace elements composition paragenesis provided information about genetic processes. This research aims at disclosing, for first time, petrographica...
During the Late Paleozoic to Cenozoic, with closure of Tethys oceans, East and/or Southeast Asia was amalgamated by individual blocks. In order understand Paleogeography Eastern Paleo-Tethys, a systematic UPb dating on 11 samples have conducted constrain age and provenance elements forming Ailaoshan-Song Ma mélange. These consist ophiolitic mélange zone (6 samples), sedimentary cover Indochina ...
The Clarke River Fault in northeast Queensland records an early Paleozoic history of subduction, accretion and continental suturing. Samples mafic–ultramafic rocks collected proximal to the record oceanic geochemical affinities comprise alteration assemblages consistent with ophiolitic origin. ca 456 Ma Falls Creek Tonalite a continental-arc signature was formed response long-lived subduction b...
The Kab Amiri area in the Central Eastern Desert (CED) of Egypt comprises ophiolitic rocks, island arc metasediments, and granitic rocks. This study deals with petrography geochemistry rocks to understand their petrogenesis geodynamic evolution CED belt. ophiolite is dismembered, comprising serpentinites metabasalt (spilite). Serpentinites have low contents Al2O3 (1.14 wt%) CaO (0.65 wt%), sugg...
We describe a potentially new species of platinum cupride–stannide mineral (PCSM) composition Pt(Cu0.67Sn0.33). It occurs in placer deposit the River Bolshoy Khailyk, southern Krasnoyarskiy kray, Russia. A synthetic equivalent PCSM was obtained and characterized. The as anhedral or subhedral grains up to 15 μm × 30 association with various platinum-group minerals, Rh–Co-rich pentlandite magneti...
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