نتایج جستجو برای: Serpentine polymorphs

تعداد نتایج: 4279  

The present article pays to some Alpine-Himalayan ophiolites of Late Cretaceous age from Darepahn area in the southern part of Nain-Baft Ophiolite belt. Whole rock processed data clearly shows that the metaperidotite rocks are silica-poor with low CaO, Al2O3, and TiO2 that reflect the predominance of olivine over calcic pyroxene in the protolithes. The considerable content of Co (85.6–124.6 ppm...

Journal: :Journal of the Mineralogical Society of Japan 1963

Journal: Desert 2020
B. Bahrambeygi H. Moeinzadeh, S.K. Alavipanah,

In this paper, we investigated two originated metamorphosed harzburgites of the metaperidotite complex from the northern part of the Gishaki area. Harzburgite rocks, as main ultramafic complexes of the studied area, were exposed in the scattered location of the area. Despite intensive alterations, harzburgitic units were discriminated using petrography and Raman spectroscopy studies of relict m...

نصرآبادی, محسن, پیغمبری, سیما, فرهنگیان, الهام ,

There are three serpentine polymorphs (Lizardite, Chrysotile and Antigorite) in the serpentinites of ophiolitic mélange of south Sahneh. Lizardite is observed as flake structure in the matrix of peridotites while antigorite is overgrown on lizardite and chrisotile development is just restricted to the micro fractures as a development is restricted to the micro fractures as golden and transparen...

حاجی علی اوغلی, رباب, مؤذن, محسن,

The ultramafic rocks from the Takht-e-Soleyman metamorphic complex, in Precambrian age, are classified as serpentinized metaperidotites and serpentinites, based on degree of serpentinization. Serpentine forms more than 90 volume% of the serpentinites. On the basis of serpentine polymorphs, textural relations and micro-structure features, variety of serpentinites are determined as massive serpen...

حاجی علی اوغلی, رباب,

The Naghadeh metamorphic complex at the West-Azerbaijan Province is located at termination of the NW Sanandaj-Sirjan Zone. Major varieties of the metamorphic rocks in this area are: amphibolites, greenschists, marbles and metaperidotites. The metaperidotites are classified into two groups, serpentinised metaperidotites and serpentinites. Orthopyroxene, clinopyroxene, olivine and spinel are the ...

2011
Stephanie S. Porter Maureen L. Stanton Kevin J. Rice

Species interactions play a critical role in biological invasions. For example, exotic plant and microbe mutualists can facilitate each other's spread as they co-invade novel ranges. Environmental context may influence the effect of mutualisms on invasions in heterogeneous environments, however these effects are poorly understood. We examined the mutualism between the legume, Medicago polymorph...

2013
Shannon P. Schechter Thomas D. Bruns

Specialization in plant host-symbiont-soil interactions may help mediate plant adaptation to edaphic stress. Our previous field study showed ecological evidence for host-symbiont specificity between serpentine and non-serpentine adapted ecotypes of Collinsia sparsiflora and arbuscular mycorrrhizal fungi (AMF). To test for adapted plant ecotype-AMF specificity between C. sparsiflora ecotypes and...

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