مم تكون جميع المواد ؟. مم تكون جميع المواد

Name: مم تكون جميع المواد ؟
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62; Levin Levin 1987 ]], pp	For descriptions of cross-bedding, see Blatt Blatt et al
For a short description of trace fossils, see Stanley Stanley 1999 ]], p	Levin Levin 1987 ]], p

93—95; and Collinson Collinson et al.

مم تكون جميع المواد: For an overview of different sedimentary environments, see or , part II
مم تكون جميع المواد: Levin Levin 1987 ]], pp
حل كتاب الاجتماعيات ثالث متوسط الفصل الثاني: For an overview over facies shifts and the relations in the sedimentary rock record by which they can be recognized, see , pp

Folk Folk 1965 ]], p	Stanley Stanley 1999 ]], p
For concretions, see Collinson Collinson et al	Stanley Stanley 1999 ]], pp

For a definition of shallow marine environments, see , p.

مم تتكون المادة: For an overview of sedimentary basin types, see , pp
مم تكون جميع المواد: For an overview of major minerals in siliciclastic rocks and their relative stabilities, see Folk Folk 1965 ]], pp
مم تكون جميع المواد: For an overview of continental environments, see , pp

: Planetary Geology Program, Office of Space Science, National Aeoronautics and Space Administration	Stanley Stanley 1999 ]], p
Boggs1987 Boggs 1987 ]], p

For a short explanation of Milankovitch cycles, see , pp.