نتایج جستجو برای: kerman cenozoic magmatic arc

تعداد نتایج: 46646  

B. Monfaredi

Tertiary andesitic basalts of the Sirjan area, Urmieh-Dokhtar Magmatic Arc, Iran, contain plagioclase phenocrysts enclosed in a matrix of amphibole, clinopyroxene and rare olivine crystals. Textural and compositional evidence suggests two significantly different types of plagioclase phenocrysts occur in the andesitic basalts. The most common type of plagioclase phenocrysts have zoning patterns ...

2017
Jamileh Farokhzadian Golnaz Forughameri Abbas Karami

Jamileh Farokhzadian, Golnaz Forughameri, Abbas Karami. Department of Community Health Nursing, School of Nursing and Midwifery, Kerman University of Medical Sciences, Kerman, Iran; Department of Community Health Nursing, School of Nursing and Midwifery, Kerman University of Medical Sciences, Kerman, Iran; MSc student of Nursing, School of Nursing and Midwifery, Kerman University of Medical Sci...

2013
Maryam Nasirian Mohammad Karamouzian Ali-Akbar Haghdoost

Regional Knowledge Hub for HIV/AIDS Surveillance, Institute for Futures Studies in Health, Kerman University of Medical Sciences, Kerman, Iran DVM, Regional Knowledge Hub for HIV/AIDS Surveillance, Institute for Futures Studies in Health, Kerman University of Medical Sciences, Kerman, Iran Regional Knowledge Hub for HIV/AIDS Surveillance, Institute for Futures Studies in Health, Kerman Universi...

2007
Zhao-Jie Guo Alexander Robinson Cheng-Zao Jia

We welcome Zhang et al.’s comment on our recent paper dealing with the significance of the first geochemical and geochronological analyses of deep drill-core samples collected from the basement of the central Tarim basin (Guo et al., 2005). In their comments, Zhang et al. raised three questions with regard to our paper (1) the compatibility of our model with regional geology, (2) our interpreta...

شبانیان بروجنی, ناهید, داودیان دهکردی, علیرضا , سهیلیان , فرنوش ,

Gabbroic pluton of Bagham is located in southeastern Ardestan and has intruded into Eocene volacanic rocks. The study area is a part of Central Iranian zone and Urumieh-Dokhtar magmatic belt. Clinopyroxene, plagioclase and amphibole are main minerals in the pluton. Mineral chemistry studies show that clinopyroxenes are augite and are plotted in almost medium pressure field. The clinopyroxene co...

زرین‌کوب, محمدحسین, محمدی, سیدسعید, خطیب, محمد‌مهدی, لین چانگ, سون,

Rich area’s sub volcanic bodies in southwest of Birjand have intruded into Upper Cretaceous ophiolite mélange.  These rocks are in diorite porphyry to monzonite porphyry range and their main texture is porphyry with microgranular groudmass. Plagioclase and green hornblende phenocrysts are made about 70% of these rocks. Plagioclases are andesine with albitic and carlsbad twining and distinct zon...

Journal: Geopersia 2019

This article provides a background for scientists interested in a general overview of the geology and geomorphology of Turkmenistan. The basement of Turkmenistan is a complex amalgamation of arc-related terranes developed in the Asiatic and northern Paleotethys oceanic domains during Late Paleozoic to Triassic times. A major part of the country coincides with the Turan Platform, where a thick s...

Journal: :Journal of Asian Earth Sciences 2021

The Avaj Oligocene volcanic – plutonic complex is part of extensive Cenozoic magmatic activity within the Urumieh-Dokhtar arc Iran. We use whole rock geochemistry, mineral compositions and crystal size distributions (CSD) in a suite co-genetic basalt, basaltic andesite gabbro to determine their petrogenesis. Ca-rich cores plagioclase (An79-86) overlap empirically modelled compositions, indicati...

Journal: :Geology 2023

Back-arc extension has been well documented in subduction plate tectonic regimes. However, the reasons why back-arc extensions are associated with some systems but not others have remained elusive. Here, spatio-temporal variations composition of Cenozoic basalts northeast Asian continental margin used to constrain mechanism for episodic extensions. Using geochemical data sensitive affinity, we ...

Journal: :Andean Geology 2021

The Cordillera Real granitoids are a suite of Triassic and Oligocene plutons in the core Eastern Central Andes Bolivia. Their tectonic setting, chemical ore compositions make them part so-called “Inner Magmatic Arc”, which differs from current “Magmatic Arc” located immediately to west. U-Pb SHRIMP data were obtained order constrain crystallization ages. group yielded following results: 239±2 M...

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