Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Hermes Panggabean"'
Autor:
Lauti Dwita Santy, Hermes Panggabean
Publikováno v:
Indonesian Journal on Geoscience, Vol 8, Iss 1, Pp 39-53 (2014)
DOI: 10.17014/ijog.v8i1.154The Ketungau and Melawi Basins, in West Kalimantan, are Tertiary intramontane basins of which the potential for economic conventional oil and gas discoveries have not previously been confirmed. The Ketungau Basin is bordere
Externí odkaz:
https://doaj.org/article/99011216ef714923845e8540c1a27da5
Publikováno v:
Indonesian Journal on Geoscience, Vol 1, Iss 1, Pp 53-64 (2014)
DOI: 10.17014/ijog.v1i1.175The Oligocene Sinamar Formation consists of shale, claystone, mudstone, sandstone, conglomeratic sandstone, and intercalation of coal seams. The objective of study was to identify the hydrocarbon source rock potential of th
Externí odkaz:
https://doaj.org/article/dd0b90bb00c14880a7dd9db7321ee899
Autor:
Kusnama Kusnama, Hermes Panggabean
Publikováno v:
Indonesian Journal on Geoscience, Vol 4, Iss 2, Pp 133-144 (2014)
http://dx.doi.org/10.17014/ijog.vol4no2.20095The rock succession of coal bearing formation, situated in Lampung Tengah, occupies the basinal margin or the western part of South Sumatra Basin. Physiographically, the rock succession lies in the Palemba
Externí odkaz:
https://doaj.org/article/890e8c085ff84be392e69d76989da5a8
Autor:
Hermes Panggabean, R. Heryanto
Publikováno v:
Indonesian Journal on Geoscience, Vol 4, Iss 1, Pp 43-55 (2014)
http://dx.doi.org/10.17014/ijog.vol4no1.20095The Tertiary Bengkulu Basin is known as a typical fore-arc basin, situated in southwest Sumatera. The basin initiated during Eocene-Oligocene times, accumulates the Lahat equivalent formation. The formatio
Externí odkaz:
https://doaj.org/article/deba998e357b47b5bd1c7d93b22a4164
Autor:
Asep Kurnia Permana, Aris Kusworo, Joko Wahyudiono, Y A. Sendjaja, Hermes Panggabean, L Fauziely
Publikováno v:
Jurnal Geologi dan Sumberdaya Mineral. 23:1-15
The Miocene sedimentary rocks in Samarinda area constrains organic rich sediments, which are considered as a good source rocks hydrocarbon in the East Kutai Sub-Basin, Kalimantan. The high organic material content within the sediments is related to t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4500b9414b27725874cba4347c5d4578
https://doi.org/10.33332/jgsm.geologi.v23i1.660
https://doi.org/10.33332/jgsm.geologi.v23i1.660
Publikováno v:
Indonesian Journal on Geoscience. 8
DOI: 10.17014/ijog.v8i1.153 The research area is situated in the northwestern side of South Sumatra Basin, which is a part of Muara Bungo Regency, Jambi Province. The Oligocene Sinamar Formation consists of shale, claystone, mudstone, sandstone, cong
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad2924c4a06bec287a2c4cbbc060bcfe
https://doi.org/10.17014/ijog.8.1.25-38
https://doi.org/10.17014/ijog.8.1.25-38
Autor:
David Ontosari, Benyamin Sapiie, Jakarta Postgraduate Alumni Fitb Itb, Hermes Panggabean, Eddy Slameto
Publikováno v:
Bulletin of Geology. 2:229-242
Area "Noken" is located in the Akimeugah Basin, southern of Papua, covering onshore and offshore areas. In previous research, this area is still defined as laterally uniform passive margin basin during Mesozoic Era. A number of data include airborne-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c0f698c4374dc40bce3c25f8d1fbdb8
https://doi.org/10.5614/bull.geol.2018.2.2.3
https://doi.org/10.5614/bull.geol.2018.2.2.3
Autor:
Iyan Haryanto, Yoga B.Sendjadja, David Victor Mamengko, Hermes Panggabean, Budi Mulyana, Eko Budi Lelono, Juwita Trivianty Musu, Panuju Panuju
Publikováno v:
Jurnal Geologi dan Sumberdaya Mineral. 20:37
North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sedim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::59c52073d552a8e3d633ab24906d2dc7
https://doi.org/10.33332/jgsm.geologi.v20i1.399
https://doi.org/10.33332/jgsm.geologi.v20i1.399
Autor:
Hermes Panggabean
Publikováno v:
Indonesian Journal on Geoscience.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd7192adc94cf2a31d68bf21179ee694
https://doi.org/10.17014/ijog.vol4no1.20095
https://doi.org/10.17014/ijog.vol4no1.20095
Autor:
Hermes Panggabean, C. J. Pigram
Publikováno v:
Nature. 301:231-234
The age of the Banda Sea is critical for palaeogeographical reconstructions of eastern Indonesia. Assumed ages for its formation range from Mesozoic to Neogene1–10. However, geophysical evidence shows that the Banda Sea is floored by oceanic crust1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ff347a9f7118e88f35bbff0bdaf40eb
https://doi.org/10.1038/301231a0
https://doi.org/10.1038/301231a0