Zobrazeno 1 - 10
of 38
pro vyhledávání: '"Deny Setiady"'
Autor:
Deny Setiady, I Wayan Lugra
Publikováno v:
Bulletin of the Marine Geology, Vol 28, Iss 2, Pp 21-29 (2017)
The study area is located at coastal and offshore Kundur and Adjacent Area, geographically located at coordinates of 0º 39'00 "0º 50'00" N and 103º 10'00 "103º 25 '00" S. Rare earth elements are found in seven seafloor surfacial sediment
Externí odkaz:
https://doaj.org/article/9ad238f882544aad9b02fc849ed25f0c
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:
I Wayan Lugra, Deny Setiady
Publikováno v:
Bulletin of the Marine Geology, Vol 27, Iss 2, Pp 99-107 (2017)
Segara Anakan Lagoon is an unique lagoon , where a lot of rivers enter into the lagoon such as Citanduy, Cibeureum, Cijolang, Cikawung and Ciseel Rivers. These rivers bring the sediment materials from upstream to the lagoon areas and resisted by Nusa
Externí odkaz:
https://doaj.org/article/6393091afdf24d00a6680dc3242f5c57
Autor:
Deny Setiady, Ediar Usman
Publikováno v:
Bulletin of the Marine Geology, Vol 30, Iss 2, Pp 67-74 (2017)
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 re
Externí odkaz:
https://doaj.org/article/f5b8fa51e5b641d888c46c66d63418d8
Publikováno v:
Bulletin of the Marine Geology, Vol 32, Iss 1 (2017)
Some deepwater multiple attenuation processing methods have been developed in the past with partial success. The success of surface multiple attenuation relies on good water bottom reflections for most deepwater marine situations. It brings the bigge
Externí odkaz:
https://doaj.org/article/4b06285670ee411baf3a6852227010d3
Autor:
Deny Setiady
Publikováno v:
Indonesian Journal on Geoscience, Vol 5, Iss 1, Pp 57-74 (2014)
DOI: 10.17014/ijog.v5i1.93Based on the depth contour, the sea bottom morphology in southern part of the researched area is very steep, while in the northern area it is sloped slightly. It shows that sedimentation process is from south to the north an
Externí odkaz:
https://doaj.org/article/2db57aa85d9340b9a2a79b177877d81b
Publikováno v:
JURNAL GEOLOGI KELAUTAN. 20
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3c314b9a7dd96e8256fe0f5cef0c499
https://doi.org/10.32693/jgk.20.2.2022.791
https://doi.org/10.32693/jgk.20.2.2022.791
Autor:
Agus Setyanto, Deny Setiady
Publikováno v:
JURNAL GEOLOGI KELAUTAN. 20
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::add2bc598937830a66dd62f41daa8c5d
https://doi.org/10.32693/jgk.20.1.2022.756
https://doi.org/10.32693/jgk.20.1.2022.756
Publikováno v:
JURNAL GEOLOGI KELAUTAN. 19
Perairan Wokam Aru Utara, Papua Barat merupakan bagian tepi utara passive margin Mesozoik Arafura – Australia. Hasil survei dengan KR. Geomarin III di perairan Wokam 2014 diperoleh lintasan seismik Multi Kanal 1.182 km, dan pemeruman batimetri/sub
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24129ce985951eaf83cbd4ae3c02f604
https://doi.org/10.32693/jgk.19.1.2021.694
https://doi.org/10.32693/jgk.19.1.2021.694
Autor:
Yogi Noviadi, Deny Setiady
Publikováno v:
JURNAL GEOLOGI KELAUTAN. 18
Pesisir Kulon Progo secara fisiografi merupakan bagian dari zona pegunungan selatan Jawa, berbatasan disebelah timur nya adalah zona Solo. Tujuan penelitian ini adalah untuk mengetahui proses sedimentasi endapan pasir pantai dan kemungkinan batuan su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::335c000761953d806ec02e5cae3c465c
https://doi.org/10.32693/jgk.18.1.2020.583
https://doi.org/10.32693/jgk.18.1.2020.583