scholarly journals usSEABED: Atlantic coast offshore surficial sediment data release

Data Series ◽  
10.3133/ds118 ◽  
2005 ◽  
Author(s):  
Jamey M. Reid ◽  
Jane A. Reid ◽  
Chris J. Jenkins ◽  
Mary E. Hastings ◽  
S. Jeffress Williams ◽  
...  
Data Series ◽  
10.3133/ds146 ◽  
2006 ◽  
Author(s):  
Brian J. Buczkowski ◽  
Jane A. Reid ◽  
Chris J. Jenkins ◽  
Jamey M. Reid ◽  
S. Jeffress Williams ◽  
...  

Data Series ◽  
10.3133/ds182 ◽  
2006 ◽  
Author(s):  
Jane A. Reid ◽  
Jamey M. Reid ◽  
Chris J. Jenkins ◽  
Mark Zimmermann ◽  
S. Jeffress Williams ◽  
...  

2006 ◽  
Vol 4 (1) ◽  
pp. 68-80 ◽  
Author(s):  
Pavlina Simeonova ◽  
Costel Sarbu ◽  
Thomas Spanos ◽  
Vasil Simeonov ◽  
Stefan Tsakovski

AbstractThe present paper deals with the application of classical and fuzzy principal components analysis to a large data set from coastal sediment analysis. Altogether 126 sampling sites from the Atlantic Coast of the USA are considered and at each site 16 chemical parameters are measured. It is found that four latent factors are responsible for the data structure (“natural”, “anthropogenic”, “bioorganic”, and “organic anthropogenic”). Additionally, estimating the scatter plots for factor scores revealed the similarity between the sampling sites. Geographical and urban factors are found to contribute to the sediment chemical composition. It is shown that the use of fuzzy PCA helps for better data interpretation especially in case of outliers.


Data in Brief ◽  
2020 ◽  
Vol 31 ◽  
pp. 105813
Author(s):  
Rafael C. Carvalho ◽  
Colin D. Woodroffe

2003 ◽  
Author(s):  
Lawrence J. Poppe ◽  
V.F. Paskevich ◽  
S.J. Williams ◽  
M.E. Hastings ◽  
J.T. Kelley ◽  
...  

2016 ◽  
Vol 30 (2) ◽  
pp. 67
Author(s):  
Deny Setiady ◽  
Ediar Usman

According to the regulation No 4 of 2009 of Mineral and Coal Mining Management stated that the requirement of an inventory for mineral resources data was created to support the establishment of mining area. This study is intended to obtain mineral resources content and surficial sediment data, Geographically the study area belongs to Meranti Archipelago Regency, Riau Province. it is located between 102o00'00" - 103o 15'00" E and 00o35'00" - 01o28'00" N. Grain size analyses result show that surficial sediment in the study area consists of silt, silty sand and sand which is dominated by silt. Based on the mineral identification, some of the minerals such as quartz, cassiterite, magnetite, hematite, dolonite, biotite and zircon have been found. Silt distribution is very wide started from estuarine southeast part northen part of Rangsang Island toward southeast of rangsang island. Sandy silt only found at the southeast of Rangsang Island, while sand sediment is found at the south and southeast of Rangsang Island. The presence of silt and sand grains is influenced by moderate to strong currents and wave patterns, so that the silt and sand grains sediment was transported along coastal to offsore area, while the fine grained (clay - silt) are deposited in the valley at the western part of Rangsang Island.Keywords: mineral, surficial sediment, Rangsang Island Berdasarkan Undang Undang Nomor 4 tahun 2009 tentang Pengelolaan Pertambangan Mineral dan Batubara, disebutkan bahwa inventarisasi data sumber daya mineral diperlukan dalam rangka mendukung penetapan Wilayah Pertambangan (WP). Penelitian ini dimaksudkan untuk memperoleh data kandungan sumber daya mineral dan sedimen dasar laut. Daerah penelitian, secara geografis termasuk dalam Kabupaten Kepulauan Meranti, Provinsi Riau, dan terletak pada koordinat antara 102o00'00" - 103o15'00" BT dan 00o35'00" - 01o28'00" LU. Hasil analisis besar butir menunjukkan sedimen permukaan dasar laut di daerah penelitian terdiri atas lanau, lanau pasiran dan pasir yang didominasi oleh lanau. Berdasarkan identifikasi mineral pada sedimen permukaan dasar lautnya menunjukkan kehadiran mineral kasiterit, magnetit, hematit, dolomit, biotit, zirkon dan kuarsa. Penyebaran lanau sangat luas dimulai dari daerah estuari barat laut dan bagian utara Pulau Rangsang, hingga ke sebelah tenggara Pulau Rangsang. Lanau pasiran hanya terdapat di tenggara Pulau rangsang, sedangkan pasir hanya terdapat di daerah di bagian selatan - tenggara Pulau Rangsang. Adanya butiran lanau - pasir dipengaruhi oleh pola arus dan gelombang yang sedang sampai kuat, sehingga butiran berukuran lanau - pasir dapat terangkut ke arah lepas pantai, sedangkan butiran halus (lempung) mengendap di daerah lembah di bagian barat Pulau Rangsang. Kata kunci: mineral, sedimen permukaan dasar laut, Pulau Rangsang


2018 ◽  
Author(s):  
D A J Stepner ◽  
A F Bajc ◽  
A K Burt ◽  
R D Knight ◽  
H A J Russell

1998 ◽  
Vol 10 (3) ◽  
pp. 227-235 ◽  
Author(s):  
P.T. Harris ◽  
F. Taylor ◽  
Z. Pushina ◽  
G. Leitchenkov ◽  
P.E. O'Brien ◽  
...  

Over the past 15 years, Japanese, Australian and Russian expeditions to Prydz Bay have collected about 30 000 km of bathymetric data, 6000 km of sidescan sonar data and more than 250 sediment grab and core samples. These data were used in the present study to compile surficial sediment, bathymetric, and geomorphological maps of the Prydz Bay region. Lithofacies distribution was determined by surficial sediment data analysis using sample matrix (Q-mode) and cluster analysis techniques based on data from 206 sites. Data included percentage biogenic silica (opal), calcium carbonate, gravel, mud, and relative abundance of two diatom species (Fragilariopsis curta and F. kerguelensis). Five lithofacies are identified from the available data: (1) slightly gravelly sandy mud (g)sM lithofacies, (2) siliceous mud and diatom ooze (SMO) lithofacies, (3) F. kerguelensis pelagic ooze lithofacies, (4) F. curta gravelly muddy sand gmS lithofacies and (5) calcareous gravel lithofacies. In many areas the lithofacies correlate to geomorphological provinces as defined by previous investigators using 3.5 kHz and sidescan sonar data. In some cases, Holocene SMO sediments are seen to drape over iceberg plough marks, implying that these are relict features. These five lithofacies are likely to dominate most of the East Antarctic shelf region and may be helpful in defining sedimentary successions resulting from ice-sheet advance and retreat over glacial-interglacial cycles.


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