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  • Mineralogy of the Major Soils of the Gezira Scheme Sudan

    Mineralogy Of The Major Soils Of The Gezira Scheme Sudan

    The coarse clay is composed of chlorite, kaolinite, smectite, plagioclase and K-feldspars, quartz, and mica. The fine clay is predominantly smectite (a mixture of montmorillonite and beidellite), kaolinite, and mica. Calcite is the dominant mineral in the gray hard nodules.

  • New ophiolite occurrences in Sudan and constraint on the

    New Ophiolite Occurrences In Sudan And Constraint On The

    Jan 01, 2011 Layered Gabbros consist of calcic-plagioclase (andesine to labrodorite), augite, hypersthene, and relicts of hornblende and olivine. There is partial to complete replacement of pyroxenes by hornblende (Plate 1E). Secondary minerals include actinolite and chlorite after mafic minerals. Iron oxides, epidote and apatite occur as accessory minerals.

  • Minerals Potential and Resources in Sudan

    Minerals Potential And Resources In Sudan

    the boundaries between nine countries Sudan has a huge mineral potential yet to be evaluated and developed. The Ministry of Minerals, through the Geological Researches Authority of the Sudan (GRAS), the State Geological Survey, is the guardian of all metals and minerals within the lands, rivers and the continental shelf of the Sudan.

  • Late proterozoic island arc volcanics from Gebeit Red Sea

    Late Proterozoic Island Arc Volcanics From Gebeit Red Sea

    The area of Gebeit Mine in the northern Red Sea Hills, Sudan, is built up of voluminous volcanic rocks and minor volcaniclastic and clastic sequences. According to their chemical and modal compositions the Gebeit volcanics can be devided into four groups (a) cpx-physic basalts with clinopyroxene and plagioclase as the dominant phenocrysts and minor opaques (b) hbl-physic basalts with ...

  • Sodium Plagioclase Geology 1501 ECU

    Sodium Plagioclase Geology 1501 Ecu

    Type Mineral Luster Nonmetallic Glassy Hardness 6 Glass Cleavage Yes Prismatic at right angles Streak None Color White to Light Gray Miscellaneous ...

  • Calcium Plagioclase Geology 1501 ECU

    Calcium Plagioclase Geology 1501 Ecu

    Type Mineral Luster Nonmetallic Hardness 6 Glass Cleavage Yes Prismatic at right angles Streak None Color Dark Gray, Blue, or Black Miscellaneous ...

  • Plagioclase UND

    Plagioclase Und

    Plagioclase and Augite in a Basalt. The photos above show abundant plagioclase lathes (clear - PP low order interference colors - XP) and the clinopyroxene augite (almost clear- PP 2nd order yellow to blue to pink interference colors-XP) in a matrix that contains a lot of brown glass.Two vesicles are also present (clear, PP isotropic, XP) -- one left of center on the bottom edge, and the ...

  • Plagioclase Mineral Data

    Plagioclase Mineral Data

    Plagioclase Labradorite. Comments Dual view of a cleavage fragment of labradorite showing the multi-colored labradorescence (schiller effect) and the same area viewed without the color.The color is due to optical interference on Bggild exsolution lamellae. Location Ihosy, Betroka district, Toliara Province, Madagascar.Scale Picture size 3x3 cm. ...

  • ALEX STREKEISENPlagioclase

    Alex Strekeisenplagioclase

    Plagioclase feldspars are the most common feldspar minerals because calcium is somewhat more common in the crust than potassium (3.6 and 2.8 percent of the crust, respectively). Plagioclase feldspars form a continuous solid solution between Ab and An endmembers at high temperature, but the replacement of ions needs to be coupled because of the ...

  • Plagioclase thin section Tectosilicates MicROCKScopic

    Plagioclase Thin Section Tectosilicates Microckscopic

    Plagioclase (series of minerals in the feldspar group), from Greek for oblique and fracture, in reference to the oblique angle between its best cleavages. Anorthite (Ca %90-100 Na %10-0) from Greek for not straight, because of its triclinic symmetry. Bytownite (Ca %70-90 Na %30-10) locality at Bytown (now the city of Ottawa), Canada. ...

  • PAPER OPEN ACCESS Petrographic investigation and

    Paper Open Access Petrographic Investigation And

    Mar 12, 2020 plagioclase). The feldsparsare highly sericited and kaolintized Muscovite and chloriteare recognized that intensively affected by deformation and forming what is called pressure shadow texture (brittle minerals bentaround the harder one like quartz and pyrite). Pyr ite is found in considerable amount due hydrothermal activities.

  • Dating of late Proterozoic ophiolites in Egypt and the

    Dating Of Late Proterozoic Ophiolites In Egypt And The

    Dating of late Proterozoic ophiolites in Egypt and the Sudan using the single grain zircon evaporation technique ... grained mosaic of plagioclase, quartz, minor ... found sericitization of plagioclase and chlori- tization of hornblende. Accessory minerals include magnetite, ilmenite, apatite and zir- con. The latter crystals are between 20 and ...

  • Plagioclase Mineral Specimen For Sale

    Plagioclase Mineral Specimen For Sale

    Plagioclase - All kinds of good play of colors in this specimen of labradorite, a variety of Plagioclase with Albite. This special breed of feldspar is an intermediate product between the compositions of Albite and Anorthosite, both plagioclase feldspars. Tilting the specimen back and forth causes an optical phenomenon known as labradorescence andis caused by several degrees of refraction ...

  • Geological and Tectonic Setting of the Kamoreib

    Geological And Tectonic Setting Of The Kamoreib

    opaque minerals of probably iron oxides are dispersed throughout the matrix in the form of fine to medium-grains and make up 0.5 to 1% of the rock. Fig. 2. Geological Map of the Komoreib Area, Red Sea Hills, Sudan The andesite is a fine-grained, highly altered rock consisting of plagioclase phenocrysts, which are completely

  • Geological and Geochemical Studies of Granitiod

    Geological And Geochemical Studies Of Granitiod

    arrangement of the ferromagnesian minerals giving the rock a gneiss appearance. They consist mainly of plagioclase feldspar, quartz, K-feldspar, hornblende, biotite, with subordinate secondary chlorite, epidote and sericite (Fig. 2.1). Accessory minerals are mainly zircon, titanite, apatite and magnetite.

  • Plagioclase The Delaware Geological Survey

    Plagioclase The Delaware Geological Survey

    Nov 17, 2010 Major minerals in the marble include calcite and dolomite with phlogopite, diopside, olivine, and graphite. Major minerals in the calc-schist are calcite with phlogopite, microcline, diopside, tremolite, quartz, plagioclase, scapolite, and clinozoisite.

  • Tectosilicates Other Minerals

    Tectosilicates Other Minerals

    State whether each of the following minerals would be most commonly found in igneous rocks, metamorphic rocks, or both igneous and metamorphic rocks (a) quartz, (b) plagioclase, (c) sanidine, (d) microcline, (e) nepheline, (f) sodalite, (g) leucite, (h) apatite. Which minerals would be good ores for Cr, Al, Fe, Ti, or Mn?

  • Mineral and Rock Guide booked CCSF

    Mineral And Rock Guide Booked Ccsf

    contain green minerals (actinolite epidote /- chlorite) gi ving it a green appearance. Formed through medium grade burial of basalt/gabbro. (Can also contain hornblende plagioclase /- garnet.) Gneiss Granite/rhyolite, shale B, R, S High Grains medium to coarse li ght and dark minerals segregated into bands. Gneissic texture.

  • PDF The Geology of Juba and the Surrounding Area

    Pdf The Geology Of Juba And The Surrounding Area

    Also gabbro is found incorporated with granite at Jebel Kunufi in southeast portion of the outcrop adjacent to the quarry. It is produced as a result of assimilation of the felsic magma by the country rock. It is composed of few light minerals and composes dominantly of biotite,

  • Chapter 3 Igneous Textures

    Chapter 3 Igneous Textures

    Hawaii. Black minerals are felsic plagioclase and gray ones are mafics. a. Large . embayed. olivine phenocryst with smaller plagioclase laths and clusters of feathery augite nucleating on plagioclase. Magnification ca. 400X. b. ca. 2000X magnification of feathery quenched augite crystals nucleating on plagioclase (black) and

  • Identification Tables for Common Minerals in Thin

    Identification Tables For Common Minerals In Thin

    Minerals with refractive indices close to 1.54 have low relief, those with much higher or lower refractive indexes will have high relief. (vi) Extinction angles are only given where minerals usually show a linear feature such as a cleavage and/or long crystal faces. For plagioclase feldspars (stippled) the extinction

  • LAB 3 COMMON MINERALS IN SEDIMENTARY

    Lab 3 Common Minerals In Sedimentary

    plagioclase. Mafic minerals readily weather to form clays and iron hydroxy-oxides, and so are uncommon in sedimentary rocks. Thus the most important minerals in clastic sedimentary rocks are quartz, potassium feldspar (microcline and orthoclase), plagioclase, clays, and oxides/hydroxy-oxides (hematite, limonite, goethite).

  • Northeast Africa 001 NASA

    Northeast Africa 001 Nasa

    Egypt-Sudan border (Fig. 2). It has no fusion crust, and extensive terrestrial alteration products around the edges and in cracks, include calcite, barite, gypsum, and Fe hydroxides. It is an anorthositic regolith breccia consisting of mineral fragments and

  • Plagioclase an overview ScienceDirect Topics

    Plagioclase An Overview Sciencedirect Topics

    Plagioclase minerals are extremely widespread and abundant. It is as essential and important constituents of many igneous, sedimentary, and metamorphic rocks, acidic, neutral, and basic, pegmatite igneous rocks, feldspar-sandstone, siltstone and shale, and amphibolite schist and gneiss (Tables 5.1 and 7.1 Table 5.1 Table 7.1).

  • Plagioclase Feldspar NOVA Mineralogy

    Plagioclase Feldspar Nova Mineralogy

    Plagioclase Feldspar. The plagioclase feldspars are those within the plagioclase solid solution series. Plagioclase feldspars are easy to identify in thin section they display first order grays and stripey twins. Youll often see plag grains covered in something that looks like dirt (PPL) or tiny confetti (XPL) that is plag caught in the ...

  • Feldspar

    Feldspar

    Plagioclase Orthoclase Feldspar is a name given to a class of aluminum-containing silicates which are sometimes called light silicates or nonferromagnesian silicates since they dont contain iron or magnesium. The feldspars include orthoclase (KAlSi 3 O 8) and plagioclase ((Ca,Na)AlSi 3 O 8).Note that the plagioclase differs from the orthoclase in terms of the additional metals, plagioclase ...

  • The Geology and Geochemistry of Metavolcanic Rocks

    The Geology And Geochemistry Of Metavolcanic Rocks

    elongated quartz and plagioclase grains. Under the microscope the gneiss shows a simple mineral assemblage composing of angular to subangular quartz crystals within predominate orthoclase feldspars and minor plagioclase (Albite- oligoclase composition) both may be altered to turbid sericite. Of the mafic minerals, oriented yellow biotite flakes

  • GeoI Lecture Notes Igneous Rocks

    Geoi Lecture Notes Igneous Rocks

    An refers to the anorthite content of the plagioclase. A plagioclase consisting of a mixture of 60% anorthite and 40% albite is therefore An60. A rock consisting of over 90% plagioclase (therefore less than 10% mafic minerals) is an Anorthosite. Anorthorsite is very common in the Adirondacks and in the lunar highlands. ANORTHOSITE

  • Anorthosite Sandatlas

    Anorthosite Sandatlas

    Anorthosite is an igneous monomineralic rock that is composed of plagioclase feldspar (over 90% of the rock is composed of this mineral). Plagioclase is a very common mineral group, more than half of the Earths crust is composed of it. Therefore it isnt really surprising that there is a rock type that is almost exclusively composed of plagioclase.

  • UNFORBIDDEN GEOLOGY

    Unforbidden Geology

    Anorthosite is composed almost entirely of plagioclase feldspar and a mafic mineral modal composition 10%, usually hornblende, pyroxene and olivine. Diorite is chiefly composed of feldspar, hornblende, biotite, and pyroxene, with a small amount of quartz (5%), and

  • Igneous Minerals Union College

    Igneous Minerals Union College

    It is commonly associated with other Ca-rich minerals like hornblende, plagioclase, and titanite. Epidote may have simple twinning, and can occur with quartz and various hydrous minerals like chlorite and sericite. Olivine is usually not associated with quartz (except in highly Fe-rich Mg-poor rocks), and is likely to be partly altered.

  • BasicsIgneous Rock Table

    Basicsigneous Rock Table

    Jun 21, 2020 Igneous rock is solidified magma. Plutonic igneous rock comes from magma that intrudes within the earth, deep underground, and cools and crystallizes there.Volcanic igneous rock originates from magma that erupts, as either lava or as tephra, and turns solid on the earths surface.. There are two categories of volcanic rock (1) the effusive (lava flow) type of volcanic rock, which

  • Northeast Africa Lunar Meteorite

    Northeast Africa Lunar Meteorite

    From The Meteoritical Bulletin No. 89 (preview). Northeast Africa 001. Found April 2002 in Sudan . Lunar meteorite (olivine-pyroxene basalt)Lunar meteorite (anorthositic regolith breccia) A brownish gray stone weighing 262 g was found by a prospector in northern Sudan near the Libya/Egypt/Sudan boundary in 2002 April.

  • ZrYNbREE mineralization associated with microgranite

    Zrynbree Mineralization Associated With Microgranite

    Oct 01, 2014 Muscovite occurs as minute crystals enclosed in plagioclase and filling the interstices between plagioclase and quartz (0.1- 0.4 mm). Sometimes it is characterized by porphyritic textures with prominent phenocrysts of both plagioclase and quartz minerals (Figures 13 B and C).

  • Petrology and Evolution of the Tehilla Igneous Complex

    Petrology And Evolution Of The Tehilla Igneous Complex

    Department of Geology, University of Khartoum, P.O. Box 321, Khartoum, Sudan ABSTRACT The Tehilla complex is a shallow-level, post-tectonic, ring structure of basic and acid intrusions of possible Lower Palaeozoic age. The basic rocks comprise an early phase of troctolites and norites emplaced in the form of a lopolith and sill bodies respectively.

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