Wadi Al Muhtadi fan was chosen for a detailed sedimentary logging as i terjemahan - Wadi Al Muhtadi fan was chosen for a detailed sedimentary logging as i Bahasa Indonesia Bagaimana mengatakan

Wadi Al Muhtadi fan was chosen for

Wadi Al Muhtadi fan was chosen for a detailed sedimentary logging as it is one of the largest alluvial fans in the area, and is well exposed (Fig. 2). Measurements of maximum particle size and bed thickness were made for specific lithofacies. Maximum particle size was calculated as an average of the long axis of the 10 largest clasts in a bed. The orientation of the a-b planes of a representative selection of clasts ranges from 10 to 15 readings. Palaeocurrents were measured from clast imbrication and occasional cross-beds.
Stratigraphic sections were measured from the main exposures in Wadi Al Muhtadi. Lithofacies associations are laterally distributed in the order of FP, FM and FD from east to west. Five sections were measured along the axial length of Al Muhtadi fan, from the fan apex eastward to the fan toe westward (Fig. 2).
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Wadi Al Muhtadi fan was chosen for a detailed sedimentary logging as it is one of the largest alluvial fans in the area, and is well exposed (Fig. 2). Measurements of maximum particle size and bed thickness were made for specific lithofacies. Maximum particle size was calculated as an average of the long axis of the 10 largest clasts in a bed. The orientation of the a-b planes of a representative selection of clasts ranges from 10 to 15 readings. Palaeocurrents were measured from clast imbrication and occasional cross-beds.Stratigraphic sections were measured from the main exposures in Wadi Al Muhtadi. Lithofacies associations are laterally distributed in the order of FP, FM and FD from east to west. Five sections were measured along the axial length of Al Muhtadi fan, from the fan apex eastward to the fan toe westward (Fig. 2).
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Wadi Al Muhtadi penggemar dipilih untuk sedimen logging rinci karena merupakan salah satu penggemar aluvial terbesar di daerah, dan juga terkena (Gbr. 2). Pengukuran ukuran partikel dan tempat tidur yang maksimal ketebalan dibuat untuk lithofacies tertentu. Ukuran partikel maksimum dihitung sebagai rata-rata dari sumbu panjang 10 clasts terbesar di ranjang. Orientasi pesawat ab dari pilihan perwakilan dari clasts berkisar 10 sampai 15 bacaan. Palaeocurrents diukur dari penyirapan klas dan sesekali lintas tidur.
bagian stratigrafi diukur dari eksposur utama di Wadi Al Muhtadi. Asosiasi lithofacies yang lateral didistribusikan di urutan FP, FM dan FD dari timur ke barat. Lima bagian diukur sepanjang sumbu dari Al Muhtadi penggemar, dari puncak kipas ke arah timur ke arah barat fan kaki (Gbr. 2).
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