نتایج جستجو برای: mafic dykes

تعداد نتایج: 2656  

Mineral paragenesis of rodingitized basic rocks of Iranian ophiolites are presented and metasomatic reactions between Ca+2 bearing aqueous fluids issued during serpentinization of host ultramafic rock – with magmatic minerals of basic rocks leading to present paragenesis of rodingites are discussed. It is concluded that Ca+2 rich aqueous fluid in equilibrium with serpentinite has high Ca+2 chem...

نقره‌ئیان, موسی, آلیانی, فرهاد , ترکیان, اشرف , دارایی‌زاده, زینب ,

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...

Journal: :Journal of Volcanology and Geothermal Research 2021

The Philippine Island Arc has a large number of volcanoes with diverse morphologies, making it an ideal location to study the factors controlling morphology and spatial distribution island arc volcanoes. We have identified 731 volcanic edifices using SRTM 30 m digital elevation model, computed their quantitative MORVOLC algorithm. Hierarchical classification by principal component (PC) analysis...

حسین زاده, محمدرضا, عامل, نصیر, مؤید, محسن, کمالی, امین اله,

The study area is located in NW of Iran, East-Azarbaidjan Province in north Varzeghan. Plagioclase, amphibole and biotite are the major minerals and sphene, apatite, and quartz are accessory minerals. The texture of these dykes are porphyrytic with fine to medium matrix. Mineral chemistry analysis revealed that the composition of Plagioclase varies from andesine to oligoclase and the biotite va...

2015
Bi-Ji Luo Hong-Fei Zhang Wang-Chun Xu Liang Guo He Yang

An integrated study involving whole-rock and Sr–Nd–Hf isotope geochemistry and zircon geochronology and trace element combined with detailed field investigation was carried out for the composite Meiwu batholith in the West Qinling orogenic belt of central China to probe the origins of its compositional diversity and its emplacement history. The batholith is composed of quartz diorite, granodior...

2016
Shichun Huang Munir Humayun

The role of a mafic component in the petrogenesis of Oceanic Island Basalts (OIBs) is highly debated. As the best studied OIB, Hawaiian lavas provide critical insights into OIB genesis. At a given MgO content, the CaO content in the melt has been used to distinguish between partial melts of peridotite and garnet pyroxenite/eclogite. However, calculations using the BATCH program show that CaO co...

Journal: :Frontiers in Earth Science 2023

The Laiyuan complex in the central North China Craton (NCC) incorporating different magmatic suites offers an excellent opportunity to investigate lithospheric evolution and cratonic destruction. However, petrogenesis tectonic implications of this suite remain debated due lack integrated studies. Here we evaluate magmatism setting assembling data from multidisciplinary investigations complex. i...

2009
Fang-Zhen Teng Roberta L. Rudnick William F. McDonough Fu-Yuan Wu

a r t i c l e i n f o Keywords: Lithium isotopes A-type granite Mafic enclave Continental crust Lithium concentrations and isotopic compositions of 39 A-type granites and mafic enclaves from 11 plutons in Northeast China and the North China craton are used to constrain their genesis and to characterize further the average composition of the continental crust. Lithium concentrations (2.8 to 80 p...

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