Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Kusnama Kusnama"'
Autor:
Kusnama Kusnama
Publikováno v:
Indonesian Journal on Geoscience, Vol 3, Iss 3, Pp 161-173 (2014)
http://dx.doi.org/10.17014/ijog.vol3no3.20085The Bobong Formation is a coarse clastic sedimentary rock succession. In the lower part, it consists of breccia and conglomerate facies, then followed by quartz sandstone with intercalations of claystone f
Externí odkaz:
https://doaj.org/article/dbeb6c89b35a4e09a41613cfb5ac9c52
Autor:
Kusnama Kusnama
Publikováno v:
Indonesian Journal on Geoscience, Vol 3, Iss 1, Pp 11-22 (2014)
http://dx.doi.org/10.17014/ijog.vol3no1.20082The Warukin Formation in Sampit area, occupying the Barito Basin, was conformably deposited on top of the Berai Formation, but unconformably lies on the Tanjung Formation, Undifferentiated Metamorphic Rock
Externí odkaz:
https://doaj.org/article/9a5fe7c56e9249b2bafb982080b3b616
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:
Suyono Suyono, Kusnama Kusnama
Publikováno v:
Indonesian Journal on Geoscience. 5
Autor:
Kusnama Kusnama
Publikováno v:
Indonesian Journal on Geoscience.
Autor:
Kusnama Kusnama
Publikováno v:
Indonesian Journal on Geoscience, Vol 3, Iss 1, Pp 11-22 (2014)
http://dx.doi.org/10.17014/ijog.vol3no1.20082The Warukin Formation in Sampit area, occupying the Barito Basin, was conformably deposited on top of the Berai Formation, but unconformably lies on the Tanjung Formation, Undifferentiated Metamorphic Rock
Autor:
Kusnama Kusnama
Publikováno v:
Indonesian Journal on Geoscience, Vol 3, Iss 3, Pp 161-173 (2014)
http://dx.doi.org/10.17014/ijog.vol3no3.20085The Bobong Formation is a coarse clastic sedimentary rock succession. In the lower part, it consists of breccia and conglomerate facies, then followed by quartz sandstone with intercalations of claystone f