Iraq, , .A. Basi - University of Wasit, M., of Basic Education, C., Wasit, (2009). SEDIMENTOLOGICAL , PETROGRAPHICAL AND CLAY MINERAIOGICAL STUDY OF. , 2(2), 84-100.
Iraq; Muzahim .A. Basi - University of Wasit; College of Basic Education; Wasit. "SEDIMENTOLOGICAL , PETROGRAPHICAL AND CLAY MINERAIOGICAL STUDY OF". , 2, 2, 2009, 84-100.
Iraq, , .A. Basi - University of Wasit, M., of Basic Education, C., Wasit, (2009). 'SEDIMENTOLOGICAL , PETROGRAPHICAL AND CLAY MINERAIOGICAL STUDY OF', , 2(2), pp. 84-100.
Iraq, , .A. Basi - University of Wasit, M., of Basic Education, C., Wasit, SEDIMENTOLOGICAL , PETROGRAPHICAL AND CLAY MINERAIOGICAL STUDY OF. , 2009; 2(2): 84-100.

SEDIMENTOLOGICAL , PETROGRAPHICAL AND CLAY MINERAIOGICAL STUDY OF

Journal Of Wassit For Science & Medicine
Article 1, Volume 2, Issue 2, 2009, Pages 84-100
Authors
; Muzahim .A. Basi - University of Wasit; College of Basic Education;
Abstract
The gravels, conglomerates and the associated sediments in the studeid area, most probaly were deposited in an alluvial –fan environment . Sedimentologically, the sediments consist of three facies association: gravel and conglomerate(facies Q1),sand and sandstone (facies Q2)and gypcrete, gypseous mud and gypseous mudstone (facies Q3).These Facies most likely represent a mid-fan deposits and their material had been transported to the fan by stream flow condition .
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