The Passive Voice.
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This short document promotes creating presentations using Haiku Deck, a tool for making slideshows. It encourages the reader to get started making their own Haiku Deck presentation and sharing it on SlideShare. In just one sentence, it pitches the idea of using Haiku Deck to easily create engaging slideshows.
PETROGENESIS OF GRANITOID ROCKS AND ORIGIN OF URANIUM MINERALIZATIONS OF UM S...
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- The older granitoids (Cycle 1) have calc-alkaline, metaluminous characteristics and were emplaced during a pre-plate collision to post-collision uplift regime.
- The younger biotite granites and perthite sub-leucogranites (Cycle 2) have calc-alkaline, metaluminous compositions and were emplaced during a late-orogenic regime.
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Impact of Structural Lineaments on Mineralized Occurrences in North Abu Rushe...
This document discusses structural lineaments in the North Abu Rusheid-Sikait area of Egypt and their impact on mineral occurrences. It finds that lineaments are arranged in two main clusters trending N-S and NW-SE/WNW-ESE, controlling emplacement of granitic intrusions. A mylonitic shear zone trending ENE-WSW separates granites from ophiolitic mélange and hosts evidence of hydrothermal activity and secondary uranium mineralization. Most mineralization is related to extensional events creating space for mineral entrapment along shear zones like the ENE-WSW zone containing fluorite, molybdenite, and others.
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TECTONIC FRAMEWORK OF EAST GABAL NUQRA AREA, SOUTH EASTERN DESERT, EGYPT
The document describes a ring dyke complex located east of Gabal Nuqra in Egypt. Three magmatic events formed the rocks in the area: 1) Granites associated with the Nubian sandstone basin formation. 2) Volcanic ring dykes post-dating the basin. 3) A trachy-basaltic flow related to Red Sea rifting. Structural analysis identified three tectonic events: 1) NE-SW extension formed the Nubian basin. 2) NW-SE extension reactivated pre-existing faults. 3) E-W to ENE-WSW faults localized ring dyke emplacement and configured the trachy-basaltic flow. Hydrothermal activity
Comparative Study Between Some Uraniferous Volcanic Rocks, Eastern Desert, Egypt
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- The volcanic rocks contain varying amounts of uranium and thorium as indicated by spectrometry results, with the Um Doweila bostonite having the highest uranium content on average.
- Primary minerals identified across the areas include quartz, feldspars and pyroxenes. Secondary uranium minerals including uranophane and zippeite are also present except in the Um Domi trachyte.
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This document summarizes the occurrence of uranium-bearing minerals in pyroclastic rocks from Um Safi, central eastern desert of Egypt. Key points:
- Pyroclastic rocks from Um Safi volcano contain elevated levels of uranium and uranium-bearing minerals due to hydrothermal alteration processes.
- Three radioactive anomalies were identified - two within pyroclastics containing secondary uranium minerals like kasolite, and one within a greisenized microgranite.
- The pyroclastic rocks experienced argillization and silicification alteration and contain higher concentrations of uranium, thorium, niobium and zinc compared to fresh rhyolite samples from the volcano.
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This short document promotes creating presentations using Haiku Deck, a tool for making slideshows. It encourages the reader to get started making their own Haiku Deck presentation and sharing it on SlideShare. In just one sentence, it pitches the idea of using Haiku Deck to easily create engaging slideshows.
PETROGENESIS OF GRANITOID ROCKS AND ORIGIN OF URANIUM MINERALIZATIONS OF UM S...
- The granitoid rocks of Um Safi area were divided into three magmatic cycles based on field relationships, petrography, and geochemistry.
- The older granitoids (Cycle 1) have calc-alkaline, metaluminous characteristics and were emplaced during a pre-plate collision to post-collision uplift regime.
- The younger biotite granites and perthite sub-leucogranites (Cycle 2) have calc-alkaline, metaluminous compositions and were emplaced during a late-orogenic regime.
- The youngest muscovite sub-leucogranites (Cycle 3) are peraluminous and
Impact of Structural Lineaments on Mineralized Occurrences in North Abu Rushe...
This document discusses structural lineaments in the North Abu Rusheid-Sikait area of Egypt and their impact on mineral occurrences. It finds that lineaments are arranged in two main clusters trending N-S and NW-SE/WNW-ESE, controlling emplacement of granitic intrusions. A mylonitic shear zone trending ENE-WSW separates granites from ophiolitic mélange and hosts evidence of hydrothermal activity and secondary uranium mineralization. Most mineralization is related to extensional events creating space for mineral entrapment along shear zones like the ENE-WSW zone containing fluorite, molybdenite, and others.
YIllescas Cover Letter Resume Combined 051815
Yesenia Illescas is applying for a position and has over 10 years of experience in project management, systems analysis, data management, and business administration. She held roles implementing software, managing projects, and ensuring data integrity at various companies. Illescas has a Master's degree in Information Systems Management and is seeking to contribute her skills and passion for business and technology to the hiring company.
TECTONIC FRAMEWORK OF EAST GABAL NUQRA AREA, SOUTH EASTERN DESERT, EGYPT
The document describes a ring dyke complex located east of Gabal Nuqra in Egypt. Three magmatic events formed the rocks in the area: 1) Granites associated with the Nubian sandstone basin formation. 2) Volcanic ring dykes post-dating the basin. 3) A trachy-basaltic flow related to Red Sea rifting. Structural analysis identified three tectonic events: 1) NE-SW extension formed the Nubian basin. 2) NW-SE extension reactivated pre-existing faults. 3) E-W to ENE-WSW faults localized ring dyke emplacement and configured the trachy-basaltic flow. Hydrothermal activity
Comparative Study Between Some Uraniferous Volcanic Rocks, Eastern Desert, Egypt
- The paper compares four volcanic areas in Egypt - Um Safi rhyolite, El-Atshan bostonite sill, Um Domi trachyte, and Um Doweila bostonite - based on their geology, mineralization, alteration processes, and spectrometry.
- The volcanic rocks contain varying amounts of uranium and thorium as indicated by spectrometry results, with the Um Doweila bostonite having the highest uranium content on average.
- Primary minerals identified across the areas include quartz, feldspars and pyroxenes. Secondary uranium minerals including uranophane and zippeite are also present except in the Um Domi trachyte.
Geochemistry of lamprophyre dykes in the Eastern Desert of Egypt
This document describes the geochemistry of two lamprophyre dykes in Egypt's Eastern Desert: one in Abu Hawis and one in Abu Rusheid. The Abu Hawis dyke is composed mainly of amphibole, clinopyroxene and phlogopite. It has relatively alkaline geochemistry and enrichment in LILE, LREE, and HFSE relative to primitive mantle. The Abu Rusheid dyke cuts mylonites and contains pyroxene, phlogopite, and other minerals. It is alkaline with enrichment in LILE, transition metals, and shows negative Eu and Ce anomalies, indicating mobilization of REEs under supergene conditions. Both dykes formed in subduction-related settings but
OCCURRENCE OF URANIUM BEARING MINERALS IN UM SAFI PYROCLASTICS, CENTRAL EASTE...
This document summarizes the occurrence of uranium-bearing minerals in pyroclastic rocks from Um Safi, central eastern desert of Egypt. Key points:
- Pyroclastic rocks from Um Safi volcano contain elevated levels of uranium and uranium-bearing minerals due to hydrothermal alteration processes.
- Three radioactive anomalies were identified - two within pyroclastics containing secondary uranium minerals like kasolite, and one within a greisenized microgranite.
- The pyroclastic rocks experienced argillization and silicification alteration and contain higher concentrations of uranium, thorium, niobium and zinc compared to fresh rhyolite samples from the volcano.
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The Passive Voice.
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