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  • 标题:The Mechanism of Sediment Depositional Environment of Core Drilling of Gilimanuk Coast, Bali and Ketapang, East Java, Based on Sediment Textures
  • 其他标题:Mekanisme Lingkungan Pengendapan Sedimen dari Pemboran Inti di Pantai Gilimanuk, Bali dan Ketapang Jawa Timur, Berdasarkan Tekstur Sedimen
  • 本地全文:下载
  • 作者:Ediar Usman ; Ediar Usman
  • 期刊名称:Bulletin of the Marine Geology
  • 印刷版ISSN:1410-6175
  • 电子版ISSN:2527-8843
  • 出版年度:2016
  • 卷号:31
  • 期号:1
  • 页码:21-34
  • DOI:10.32693/bomg.31.1.2016.343
  • 语种:English
  • 出版社:Marine Geological Institute of Indonesia
  • 摘要:The analysis result of grains frequency curve and relation between grains size to cumulative have shown medium grains at Gilimanuk (Core drilling-1) and coarse grains at Ketapang (Core drilling-2). In general both of them are showed by pattern uniformity, which is represented by the similar of curve pattern. On the grain size of -2 phi as medium gravel with percentage between 6.47 to 35.88%, while core drilling -2 on the size of -2 phi between 6.86 to 61.11%.The average grains size of core drilling -1 are gravel about 21.3%, sand 60.2%, silt 5% and clay about 0.4% while core drilling-2 are characterized by 44.3%, sand 26.8%, silt 24.6% and clay about 0.6%. These result shows that at location of Core drilling -1 is dominated by sand where as at location of Core drilling -2 is dominated by gravel. These situation can be interpreted that the sediment at core drilling -2 location have influenced by strong marine current which can transport the large amount of gravel size compare to the location of Core drilling-1 which is dominated by sand. Based on the relation shape of grains size curve versus cumulative frequency shows that the sediment of Core drilling1is interpreted as a beach sand deposits and only one sample which shows as a river sand deposits which was found at depth 0 – 3 m depth. In general, the sample of Core drilling –2 shows that the pattern of sediment tend as a beach sand deposits and only one sample which shows the combination between coastal deposits and river deposits ( 4 – 5 m depth). From this sample, the coarse to fine grains is deposited by coastal media and fine grains material (about 10%) is deposited by river media. The sample of river deposits is found as lamination because the only one which is created from combination between coastal and river depos its from all sample of core drilling-2.
  • 其他摘要:Hasil analisis menggunakan kurva frekuensi butiran serta hubungan antara besar butir terhadap kumulatif menunjukkan dominasi ukuran butiran sedang di daerah Gilimanuk (Bor-1) dan kasar di daerah Ketapang (Bor-2). Pada kedua daerah tersebut, secara umum me
  • 关键词:core drilling;grain sediments;media transport;environmental deposition
  • 其他关键词:pemboran inti;butiran sedimen;media transport;lingkungan pengendapan
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