Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Noor C.D. Aryanto"'
Autor:
Deny Setiady, Noor C.D. Aryanto
Publikováno v:
Bulletin of the Marine Geology, Vol 25, Iss 1, Pp 13-21 (2017)
Placer deposits are physically accumulated by fluvial and marine processes in coastal area. Thirty six samples were selected from seventy seven samples of seafloor sediment of Singkawang waters. Those samples have been analyzed microscopically for he
Externí odkaz:
https://doaj.org/article/7322770a8ecd40df8e449e7659b946b3
Autor:
Noor C.D. Aryanto, Yani Permanawati
Publikováno v:
Bulletin of the Marine Geology, Vol 24, Iss 1, Pp 25-35 (2017)
The identification of quality and condition of the coral reef in the study areas will support the biological diversity and it frequently contains a valuable assortment of natural resources, conservation of marine biota. The environmental problem part
Externí odkaz:
https://doaj.org/article/4f84e18a56db4c508a0c1a231f06f56d
Publikováno v:
Bulletin of the Marine Geology, Vol 29, Iss 1, Pp 43-52 (2017)
Observations of coastal characteristics, such as coastal constituent lithology, oceanographic processes and the influence of human activities along the coastal area, are the factors that affect the coastal typology. The typology of coastal area can b
Externí odkaz:
https://doaj.org/article/7ca3c0c25de94c8e8f9013bebfa64c1c
Autor:
Hananto Kurnio, Noor C.D. Aryanto
Publikováno v:
Bulletin of the Marine Geology, Vol 25, Iss 2, Pp 65-76 (2017)
Strata box seismic records were used to analyze sub-seabottom paleochannels in Singkawang Waters, West Kalimantan. Based on the analyses, it can be identified the distribution and patterns of paleochannels. Paleo channel at northern part of study are
Externí odkaz:
https://doaj.org/article/cdd94eefbaf1480cae27df478e41d896
Publikováno v:
Bulletin of the Marine Geology, Vol 29, Iss 2, Pp 53-59 (2017)
South Makassar Strait is located between Kalimantan and Sulawesi Islands that is an important oceanographic pathway connecting between the Pacific and Indian oceans. This area is a part of sedimentary basin that has specific seabed morphology and sed
Externí odkaz:
https://doaj.org/article/25e246e124e84c86af11499d1ae73980
Publikováno v:
Bulletin of the Marine Geology, Vol 22, Iss 1, Pp 1-15 (2017)
Microfauna (ostracoda and foraminifera) as component of sediments has been used to detect the dynamics of sea floor condition in NE Kalimantan, particularly off Nunukan and Sebatik Islands. In general, the microfaunal components tend to increase (bot
Externí odkaz:
https://doaj.org/article/00b934ddcad3415383cd24a837e9c3a6
Autor:
Hananto Kurnio, Noor C.D. Aryanto
Publikováno v:
Bulletin of the Marine Geology, Vol 26, Iss 2, Pp 65-84 (2017)
In the history of Quaternary geology, global climate changes influenced worldwide sea-level variations. On this study, these phenomena are tried to be assessed through sea-bottom morphology changes using bathymetric and seismic strata box data obtain
Externí odkaz:
https://doaj.org/article/c94c454a861042089b3e574eaf6f9a0c
Autor:
Noor C.D. Aryanto, E. Suparka
Publikováno v:
Bulletin of the Marine Geology, Vol 28, Iss 1, Pp 13-20 (2017)
The aim of this study is to identify of petrology characteristic based on geochemical analysis in order to know the granitoid rock type. Administratively, the study area is in the City and District of Singkawang, West Kalimantan Province, at coordina
Externí odkaz:
https://doaj.org/article/49ef9e1fd85e4c8a8801afb38b3672ee
Autor:
Rohendi Rohendi, Noor C.D. Aryanto
Publikováno v:
Bulletin of the Marine Geology, Vol 27, Iss 1, Pp 7-18 (2017)
Thirty seafloor of sediment samples have been taken by using gravity corer and grab sampler at Betumpak Cape, and adjacent area of Bangka Belitung. The result of grain size analyses show that there are four sediment units: gravelly sand, gravelly mud
Externí odkaz:
https://doaj.org/article/269369678dd14296aa29fba1a44e37f3
Autor:
Hananto Kurnio, Noor C.D. Aryanto
Publikováno v:
Bulletin of the Marine Geology, Vol 28, Iss 2, Pp 13-20 (2017)
Sea floor sediment surrounding Lemukutan Island, West Kalimantan is distributed on rather steep sea bottom morphology. The steep bottom seems a continuation of rugged morphology of the island, especially at the northeast and southeast parts. This pap
Externí odkaz:
https://doaj.org/article/7f1fc594ecdc43338d6c7a22dd460405