dalam suatu cekungan dan mengetahui keterdapatan minyak dan gas bumi tersebut dengan 2) Gerakan Relatif dari Lempeng (Koesoemadinata, ). Geologi Minyak Bumi – Download as PDF File .pdf), Text File .txt) or view menganalisis struktur geologi daerah cekungan minyak minyak dan gas bumi bumi yang ada di Indonesia dengan % benar Referensi: [1] Koesoemadinata . Anna, L.O., , Geologic Assessment of Undiscovered Oil and Gas in the. Powder River Basin Koesoemadinata, R. P. , Geologi Minyak dan Gas Bumi.

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Koesoemadinata, R. P.

The Rembang area is a well-known prospective region for oil and gas exploration in Northeast Java, Indonesia. Eight lithofacies were identified from five measured stratigraphic sections, and are dominated by foreshore and tide-dominated shoreface facies.

Vol 1 No 01 References [1] Bradford, John H. Scientific Research An Academic Publisher. References [1] Bemmelen, R.

P Koesoemadinata Book 1 edition published in in English and held by 1 WorldCat member okesoemadinata worldwide. P Koesoemadinata Book 1 edition published in in Indonesian and held by 1 WorldCat member library worldwide. AAPG Memoir 26, p.

Information from the geological data shows that the Cikung field has the complex structure which is characterized by carbonate kooesoemadinata. In this episode, there is a change in depositional setting from bathyal to middle neritic.


Thus, these sandstones exhibit well to excellent reservoir qualities. Stratigraphy and petroleum occurrence: The results showed that the thickness of the reservoir in Cikung Field, estimated to range from 71 meters to meters with the prospect reservoir is at a depth of meters to meters from the surface.

P Koesoemadinata Book 1 edition published in in English and held by 2 WorldCat member libraries worldwide. Petrographic observations and grain size data indicate that these sandstones bumu texturally quite mature, based on their good-sorting and the occurrence of minor amounts of matrix clays. Nainggolan, and Nanang Dwi Ardi. Common clays in the samples include illite, smectite, kaolinite, and gibbsite.

Abstract This paper defines the stratigraphic sequence focused on Middle Baong Sand.

The Geology of Indonesia. Geologi minyak dan gasbumi by R. These sandstones are mainly composed of quartz, orthoclase, plagioclase, and micas with minor amounts of clay minerals, and therefore are predominantly classified as sub-lithic arenite and sub-felds pathicarenite. ITB, Bandung, p.

Koesoemadinata, R. P. [WorldCat Identities]

Therefore, it is required in the domain depth migration PSDM using interval velocity model is sensitive to variations in vertical and horizontal velocity to identify the thickness of the reservoir and estimation of hydrocarbon reserves. Published by UIR Press. London, print in Northern Ireland [8] Koesoemadinata R.


The porosity of the Ngrayong sandstones ranges from This paper defines kofsoemadinata stratigraphic sequence focused on Middle Baong Sand.

English 8 Indonesian 4 Malay 4. Part A by R. These sandstones are grain- and matrix-supported, and composed of very fine to medium, sub-angular to poorly-rounded, moderately- to very well-sorted sand grains. The analyses aim to understand the sedimentation pattern regarding to sequence stratigraphy model including its lateral and vertical koesoeadinata based on seismic and well data.

P Koesoemadinata Book 2 editions published in in Indonesian and held by 16 WorldCat member libraries worldwide Sociopolitical conditions in Indonesia; collection of articles previously published in Media Indonesia newspaper. P Koesoemadinata Book 4 editions published between and in Malay and held by 10 WorldCat member libraries worldwide. Clastic origin of this deposits were interpreted came from South-South West direction or from Bukit Barisan where at that time is started to uplift.

The study can be used in ranking the prospect for new oil field.