Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Eddy Mirnanda"'
Publikováno v:
Bulletin of the Marine Geology, Vol 35, Iss 1 (2020)
Fragments of ultramafic, metamorphic, basalt and serpentine compose coastal sediments. These fragments derived from outcrops in hinterland as well as the coast. Existence of greywacke sandstone through microscopic observation in coastal sediments ind
Externí odkaz:
https://doaj.org/article/2d4d729b5af84462b3b509adf7ca156a
Autor:
Tumpal Bernhard Nainggolan, Dida Kusnida, Eddy Mirnanda, Imam Setiadi, Erwin Hariyanto Nugroho, Subagio Subagio
The Central Sumatra Basin is a vast sedimentary basin and has been proven to produce hydrocarbon; this basin consists of several different sub-basins that cannot be well-imaged with conventional seismic reflection section and limited well log data. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::db2c2bca397e07f10b5cf73efa2f7d78
https://doi.org/10.21203/rs.3.rs-2837500/v1
https://doi.org/10.21203/rs.3.rs-2837500/v1
Publikováno v:
BULLETIN OF THE MARINE GEOLOGY. 37
The South Sumatra Basin is a prolific oil and gas basin. The Tulung Selapan area, which is to the east and part of the South Sumatra Basin, is considered to have hydrocarbon potential. Several sub-basins, including the South Palembang and the North P
Publikováno v:
JURNAL GEOLOGI KELAUTAN. 18
Penelitian gayaberat laut telah dilakukan di perairan Kepulauan Kai dan sekitarnya pada tahun 2018 dengan menggunakan kapal survei Geomarin 3. Tujuan penelitian adalah untuk memperoleh data geofisika kelautan dan menentukan keberadaan serta keterdapa
Autor:
Eddy Mirnanda
Publikováno v:
INDONESIAN JOURNAL OF APPLIED PHYSICS. 11:223
South China Sea (SCS) is underlain by sediments of an average density 2.10 g/cm3 of 2 km thickness at its central part up to 10 km in the margins. The basement rock is the upper and lower crust of densities 2.67 and 2.85 g/cm3 respectively of varying
Autor:
Eddy Mirnanda
Publikováno v:
INDONESIAN JOURNAL OF APPLIED PHYSICS. 10:97
Cekungan Barito agak lonjong dengan poros utama berarah Timurlaut - Baratdaya. Penampang cekungan tidak simetris, sayap bagian timur terjal sedang sayap barat relatip datar. Tepat di bagian poros utama cekungan dengan nilai anomali sekitar -25 mGal,
Autor:
Lucki Junursyah, G. M., Harja, Asep
Publikováno v:
AIP Conference Proceedings; Sep2013, Vol. 1554 Issue 1, p257-260, 4p, 4 Graphs, 1 Map