نتایج جستجو برای: clinopyroxene

تعداد نتایج: 784  

Journal: :The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists 1970

Journal: :Contributions to Mineralogy and Petrology 1983

2006
M. C. Domeneghetti A. M. Fioretti F. Camara G. Molin C. McCammon

METEORITE: SINGLE-CRYSTAL XRD, ELECTRON MICROPROBE AND MÖSSBAUER ANALYSES OF CLINOPYROXENE. M.C. Domeneghetti, A.M. Fioretti, F. Camara, G. Molin , C. McCammon . 1 Dipartimento di Scienze della Terra, Università di Pavia,Via Ferrata 1, 27100-Pavia, Italy, ([email protected]), CNR – IGG, Corso Garibaldi 37, 35137-Padova, Italy, 3 CNR – IGG, Via Ferrata 1, 27100-Pavia, Italy, 4 Dipart...

محمدی, سیدسعید, زرین کوب, محمدحسین , سلیمی, زهره ,

The study area is located in northwest of Birjand, northern part of the Sistan suture zone in eastern Iran. There is well preserved outcrops of an ophiolite mélange in this area. This complex is composed of harzburgite, layered gabbro and spilitic basalt with flysch type rocks. Microprobe analyses of olivine, clinopyroxene, orthopyroxene and spinel in harzburgites show that olivine is forsterit...

2006
N. Shirai

Introduction: It is well known that shergottites have a large variation of rare earth elements (REEs) abundance patterns and isotopic compositions. Jones [1] and Borg and Draper [2] suggest that light REEs (LREEs)-enriched shergottites resulted from mixing of a LREEs-enriched component with their parental magma. The LREEsenriched component is thought to be either Martian crust [1] or a KREEP-li...

Petrography and chemistry of minerals showing that Eocene alkaline volcanic rocks in southwestern of Germi (Talesh zone, NW Iran) mostly have basaltic composition. Mineralogically these rocks are composed of diopsidic clinopyroxene and labradoritic plagioclase phenocrysts. The microlithic and glassy groundmass composed of sanidine, clinopyroxene, biotite, pargasitic amphibole and magnetite asso...

2004
H. B. West M. O. Garcia F. A. Frey A. Kennedy

Most Hawaiian basaltic shield volcanoes are capped by moderately to strongly evolved alkalic lavas (MgO < 4.5 wt. %). On M auna Kea Volcano the cap is dominantly composed of hawaiite with minor mugearite. Although these lavas contain dunite and gabbroic xenoliths, they are nearly aphyric with rare olivine and plagioclase phenocrysts and xenocrysts. The hawaiites are nearly homogeneous in radiog...

نمودار تعداد نتایج جستجو در هر سال

با کلیک روی نمودار نتایج را به سال انتشار فیلتر کنید