Petrological Study of Clay deposits of the Lower Cretaceous in Northern of South Palmyra Folding Zone-Syria
published by Aِl-Baath University
in 2015
in
and research's language is
العربية
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Abstract in English
The Petrological study of Clay deposits belonging to the lower
Cretaceous in the northern part of South Palmyra Folding Zone.
Showed they were formed as a result of weathering processes of
igneous rocks within Sedimentary continental climate is hot and wet
conditions, and formed lateritic iron soil, followed by enrich,
erosion and washing caused by watery agitate and re-replaced for
short distances within valleys or grooves or local karst cavities, and
later filled by crust erosion materials through the Cretaceous Sea
transgression.
References used
BREW, G.;BARAZNGI, M.; Al-MALEH, K. and SAWAF,t .(2001): Tectonic and Geologic Evolution of Syria. Geo Arabia, Bahrrain, Vol.6.N0.4,573p
EBEREL, D.D. (1984): Clay Mineral Formation and Transformation in Rocks and Soils. 241-257p Great Britain
LOGVENINCO, N.V.(1984): Petrography of Sedimentary Rocks ,with bases of methology High school, Moscow, U.S.S.R .Third edition .416 p