Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Panuju Panuju"'
Autor:
Ediar Usman, Panuju Panuju
Publikováno v:
Bulletin of the Marine Geology, Vol 28, Iss 2, Pp 1-11 (2017)
Banggai-Sula Basin is one of the basins with character of the micro-continent derived from northern part of Australia. Some traces the migration in the central part of Papua are slate, schist, and gneiss, current movement is facilitated by the Sorong
Externí odkaz:
https://doaj.org/article/8aaf364388b04650abce29e37ce1ce89
Autor:
Panuju Panuju
Publikováno v:
Indonesian Journal on Geoscience, Vol 6, Iss 1, Pp 51-68 (2014)
DOI: 10.17014/ijog.v6i1.115The massive change in calcareous nannoplankton assemblages throughout Cretaceous/Tertiary (K/T) boundary (65.5 M.a.) has been illustrated by several authors. The diverse and abundant assemblage disappears suddenly above the
Externí odkaz:
https://doaj.org/article/add15a3dda8340399f4e5957d11e9346
Autor:
Panuju Panuju
Publikováno v:
Scientific Contributions Oil and Gas. 32:143-149
Waipoga-Waropen Basin is placed in northern part of Papua on the island of New Guinea. The gas discoveries had been made since 1958 in this basin, however, no economic value of reserves lead to the not producing basin state until this time. The main
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb995f53b3bcb2f007b415be09899190
https://doi.org/10.29017/scog.32.2.844
https://doi.org/10.29017/scog.32.2.844
Autor:
Panuju Panuju
Publikováno v:
Scientific Contributions Oil and Gas. 32:179-192
Lithological complexity and intense hydrocarbon exploration with the objective of Late Miocene sediments in Kutei Basin has provided the impetus for more refined Late Miocene nannoplankton zonation than the standard global schemes of Martini (1971).
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8794024dca613bb145e94537e8f6d79
https://doi.org/10.29017/scog.32.3.849
https://doi.org/10.29017/scog.32.3.849
Publikováno v:
Scientific Contributions Oil and Gas. 38:213-223
South and Central Palembang Sub - basin over Talang Akar (TAF) and the Lemat/Lahat Formations (LEF/LAF) has shale hydrocarbons (HC shale) which are considerably promising. Seismic interpretation results shows potential HC shale scattered in several a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::73cad0e660287546ed2d185dc0bf6dfd
https://doi.org/10.29017/scog.38.3.549
https://doi.org/10.29017/scog.38.3.549
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:
Panuju Panuju
Publikováno v:
Indonesian Journal on Geoscience, Vol 6, Iss 1, Pp 51-68 (2014)
DOI: 10.17014/ijog.v6i1.115The massive change in calcareous nannoplankton assemblages throughout Cretaceous/Tertiary (K/T) boundary (65.5 M.a.) has been illustrated by several authors. The diverse and abundant assemblage disappears suddenly above the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89140de3446f5d76700e830a1f276c0d
https://doi.org/10.17014/ijog.v6i1.115
https://doi.org/10.17014/ijog.v6i1.115