Based on the field observations as well as aerographical study, the plagiogranites of the ophilit... more Based on the field observations as well as aerographical study, the plagiogranites of the ophilitic sequence of Anarak, Ashin-Zavar and Nain show that these rocks have identical brecciated granular, granophyric and graphic texture. From the mineralogy point of view. quartz, ...
In north of Chah Zard farm, Jandaq metamorphic complex contains schising and marble underlay the ... more In north of Chah Zard farm, Jandaq metamorphic complex contains schising and marble underlay the amphibolites. Amphibolites are metamorphosed basalts of Jandaq ophiolite. and Jandaq metamorphic rocks are metasedimentary cover of Jandaq metaophiolite. Ampbibolites ...
Abstract Lamprophyric stocks and pillow lavas are situated in the southeast of Anarak (Isfahan Pr... more Abstract Lamprophyric stocks and pillow lavas are situated in the southeast of Anarak (Isfahan Province), adjacent to the Turkmeni-Ordib fault. Rock-forming minerals are amphibole (kaersutite), plagioclase (oligoclase and
Mantle peridotites are one of the most important rock units of Jandaq ophiolite that are affected... more Mantle peridotites are one of the most important rock units of Jandaq ophiolite that are affected by numerous phases of dynamic and static serpentinization, and metamorphism. The main part of mantle peridotites is lherzolite. This ophiolitic association is covered by Paleozoic ...
Abstract The area of study is in the North of khur and North-East of Arusan-e-kur-e-Gaz, which in... more Abstract The area of study is in the North of khur and North-East of Arusan-e-kur-e-Gaz, which in geology divisions is in Central Iran. In petrographic study intrusive body, aplitic dikes and enclaves are alkali granite. Minerals of alkali granites are K-feldspar (orthoclase ...
Jandaq ophiolite suites are covered by metamorphic rocks that are marbles and schists. This old o... more Jandaq ophiolite suites are covered by metamorphic rocks that are marbles and schists. This old ophiolitic association has passed different phases of serpentinization and metamorphism. In this rock association, gabbroic dikes cross cut the serpentinized mantle ...
Based on the field observations as well as aerographical study, the plagiogranites of the ophilit... more Based on the field observations as well as aerographical study, the plagiogranites of the ophilitic sequence of Anarak, Ashin-Zavar and Nain show that these rocks have identical brecciated granular, granophyric and graphic texture. From the mineralogy point of view. quartz, ...
In north of Chah Zard farm, Jandaq metamorphic complex contains schising and marble underlay the ... more In north of Chah Zard farm, Jandaq metamorphic complex contains schising and marble underlay the amphibolites. Amphibolites are metamorphosed basalts of Jandaq ophiolite. and Jandaq metamorphic rocks are metasedimentary cover of Jandaq metaophiolite. Ampbibolites ...
Abstract Lamprophyric stocks and pillow lavas are situated in the southeast of Anarak (Isfahan Pr... more Abstract Lamprophyric stocks and pillow lavas are situated in the southeast of Anarak (Isfahan Province), adjacent to the Turkmeni-Ordib fault. Rock-forming minerals are amphibole (kaersutite), plagioclase (oligoclase and
Mantle peridotites are one of the most important rock units of Jandaq ophiolite that are affected... more Mantle peridotites are one of the most important rock units of Jandaq ophiolite that are affected by numerous phases of dynamic and static serpentinization, and metamorphism. The main part of mantle peridotites is lherzolite. This ophiolitic association is covered by Paleozoic ...
Abstract The area of study is in the North of khur and North-East of Arusan-e-kur-e-Gaz, which in... more Abstract The area of study is in the North of khur and North-East of Arusan-e-kur-e-Gaz, which in geology divisions is in Central Iran. In petrographic study intrusive body, aplitic dikes and enclaves are alkali granite. Minerals of alkali granites are K-feldspar (orthoclase ...
Jandaq ophiolite suites are covered by metamorphic rocks that are marbles and schists. This old o... more Jandaq ophiolite suites are covered by metamorphic rocks that are marbles and schists. This old ophiolitic association has passed different phases of serpentinization and metamorphism. In this rock association, gabbroic dikes cross cut the serpentinized mantle ...
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