Enter your keyword

2-s2.0-85035123918

[vc_empty_space][vc_empty_space]

Multivariate statistical analysis for characterization of sedimentary facies of Tarakan sub-basin, North Kalimantan

Nugroho S.H.a, Putra P.S.a, Yulianto E.a, Noeradi D.b

a Research Centre for Deep Sea, Indonesian Institute of Sciences (LIPI), Ambon, Indonesia
b Department of Geology, Institut Teknologi Bandung, Bandung, Indonesia

[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]© 2017, © 2017 Taylor & Francis.A study of sediment dynamics has been conducted on the Tarakan sub-basin, North Kalimantan, Indonesia using multivariate analysis. Multivariate statistical techniques can be used to determine sediment with similar characteristics and be a good proxy to recognize sedimentary facies and depositional environment. These methods have been applied to characterize the sedimentary facies at Tarakan sub-basin. A total of 23 samples were taken from several locations on the different depths of 56–2554 m that represent varieties of environment. The study is interpreted using compositional data analysis associated with a grain size trend analysis (GSTA), principal component analysis (PCA), and cluster analysis (CA). The GSTA value showed the dominance of poorly sorted silt indicating that the sediment is mostly deposited in low-energy depositional. The CA and the PCA determined three distinct sedimentary facies: shelf facies, upper bathyal facies, and lower bathyal facies. The facies were grouped as similar sediment and depositional environment. Sedimentological variables applied in the characterization were described to be an important tool for the interpretation of depositional environments–indirectly showing hydrodynamic energy.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Depositional environment,facies,Grain size,Multivariate statistical analysis,Sediment dynamic,Tarakan[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Depositional environment,facies,grain size,multivariate statistical analysis,sediment dynamics,Tarakan[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text]We would like to thank the Indonesia Endowment Fund for Education (LPDP) for supporting and funding this research (contract number 0007016/TK/M/5/lpdp2013). We are grateful to Dr. Priatin Hadi Wijaya from Marine Geological Institute, Indonesia who gave the opportunity to use the samples. We also thank to Laboratory of Marine Geological Institute, Cirebon, Indonesia and Sedimentology Laboratory, Research center for Geotechnology, Indonesian Institute of Sciences (LIPI) for performing the sedimentology preparation and analysis. We also would like to thank Tegar Maulana, Anis Kurniasih and Reddy Setyawan for their assistance in sampling and drafting during this study. This paper is dedicated to Dr. Ir. A. Tjipto Rahardjo who passed away by the end of this study[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text]https://doi.org/10.1080/1064119X.2017.1399178[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]