TY  - BOOK
AU  - Mostafa Mohamed Omar Mohamed Hassan Elwakil
AU  - Ahmed A. Elkammar , 
AU  - Mohammad Fathy Abdelfattah , 
AU  - Yasser Medhat Abdelrahman , 
TI  - Rare elements signature of stream sediments of East Wadi Karim, South West Quseir, Eastern Desert, Egypt / 
PY  - 2018///
CY  - Cairo : 
PB  - Mostafa Mohamed Omar Mohamed Hassan Elwakil , 
KW  - Arabian-Nubian Shield
KW  - Heavy mineral
KW  - Non-opaque
N1  - Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology; Issued also as CD
N2  - Hamadat area represents the catchment zone of an elliptical diaper-like intrusion pluton trending  NNW-SSE. This pluton is one of the granitic diaper series exposed along the road that have yielded  ages between 590 and 597 Ma. It is composed mainly of K-feldspar (22-52 vol.%), plagioclase (13-45  vol.%), quartz (19-39 vol.%), and biotite (up to 12 vol.%). Based on this modal composition, it is  classified as monzogranite and it is highly jointed and exfoliated. Pegmatite and quartz veins and pods  dissect it. It is also considered as homogenous, in terms of composition. Riebeckite-bearing granite is  recorded in the northwestern segment of the pluton and it is composed mainly of perthite (up to 55%),  quartz (35-40%), albite (5-15%), riebeckite (<5%) and biotite (<5%) and commonly sheared and  highly silicified.  The recorded non-opaque heavy minerals in the studied stream sediments include biotite,  hornblende, riebeckite, epidote, and garnet, together with the accessory minerals; zircon, rutile,  titanite, tourmaline, monazite and xenotime. Thorite, allanite, monazite, zircon, and apatite are  recorded in the heavy mineral fraction as REE-bearing minerals
UR  - http://172.23.153.220/th.pdf
ER  -