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Register a new userNew data about Physical characteristics of Tripoli deposits in Palmyra Area (North 0f Sawwanet El-Hamra - North of Ghadir El-Hamal-Syria) and its economic importance
معطيات جديدة عن الخصائص الفيزيائية لتوضعات التريبولي في المنطقة التدمرية (شمال الصوانة الحمرا – شمال غدير الحمل – سورية) و أهميتها الاقتصادية
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يمثل التريبولي في منطقة الدراسة صخراً رسوبياً سيليسياً مكوناً من كوارتز مجهري التبلور، خفيف الوزن و مسامياً يلاحظ تدرج في تماسكه من سائب الى متماسك. تبين أّنه نشأ عن سيلسة الحجر الكلسي و يتكون بشكل رئيسي من كوارتز مجهري التبلور فضلاً عن بعض الشوائب من الكالسيت و الهاليت و تراوح نسبة السيليس فيه بين % 96.75 - 63.01.
Tripoli in the studied area is a porous, friable and lightweight siliceous sedimentary rock composed mainly of microcrystalline quartz, and were found to be resulting from silicification of limestone, and consists of microcrystalline quartz and impurities of calcite and halite; the silica ratio ranged between 63.01 – 96.75 % .
References used
Berg, R. B & Masters, J. M. (1994). Geology of microcrystalline silica (Tripoli) deposits. Southern Illinois. Gol. Survey. Circ. 555:89p, 55fig, 6tab 1 pl, :Champaign,111
Harben, P: Tripoli and Novaculite. (1983). The Little Known Relation. Industrial Minerals, Jan, 184 :28-32 ,4 tab London
Hunting geology and geophysics LTD (1975). Mineral exploration and development in Syria . 140-150p
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The landslides and avalanches formations represent serious
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to constitute a constructive system in some cases. Therefore appear
the importance of this study, which focused on the
tectonic role of
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deposits, mostly volcano- sedimentary of Ophiolitic complex. The
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Bassit forest
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