Salawati basin pdf editor

A new challenge and opportunity for hydrocarbon exploration in pretertiary basement. The salawati basin of western new guinea and the tomori basin of eastern sulawesi, indonesia, are two sedimentary basins located either side of the main fault strands in the sorong fault zone. The spatial analysis of satluj basin, himachal pradesh, india. Source rocks study and thermal modelling in salawati basin, west. Figure 1 is a map of the samish subbasin showing the location and site id number of each feature inventoried. The stratigraphy in a sedimentary basin is the result of the interplay of the generation of space or accommodation and the influx of sediments sediment supply.

Finally, complete content and organizational editing. Geological survey editorial standards and stratigraphic nomenclature 1988. Its not free, but if you need to edit and create pdfs professionally, adobe acrobat pro dc is the software for you. The large, mature, intracratonic, early jurassic to albian early cretaceous surat basin occupies 300 000km 2 of central southern queensland and central northern. The study area namely walio area is located at the kepalaburung psc in onshore salawati basin, west papua, indonesia fig 1. P 368 evidences of multiple phases of basin inversion in narmada block, south cambay basin, gujarat, india rajeev mohan 1, s. The efforts were rewarded with 35 commercial discoveries. Canadian well logging society, 1985, log analysis handbook. Subsurface characterization and hydrocarbon resource evaluation were conducted using integrated well logs analysis and threedimensional 3d seismicbased reservoir characterization in an. This area shows the relationships between the north misoolsorong fault, the.

Potential of prekais formation as a source rock in the salawati basin, bird head, west papua, indonesia pireno, gadjah e. Type logs and analysis for major canadian oil and gas fields. Shell oil company quit the salawati basin of irian jaya, indonesia in 1960 after drilling 30 wells in the basin over 25 years, and finding only the klamono field 33 mmboe mmboe and two subeconomic. The movement of sfz involves rotation and translation that separates salawati basin from the birds head. Canadian well logging society, variously paginated. Pdf this paper quantifi es the fl exural subsidence expected from loading by a volcanic arc. Thermal modeling and heat flow density interpretation of the. The deformed zone of the leftlateral sorong fault separates the basin with the.

Theres 3 ways to see these gorgeous units online or phone for your private inspection. Paper open access seismic interpretation and depositional. Sedimentary basin analysis involves studying the history of sediment accumulation within depocenters and the tectonic processes that create the basin depression, influence the distribution of sediments. Basin analysis is an advanced undergraduate and postgraduate text aimed at understanding sedimentary basins as geodynamic entities. Tba field is an offshore field located in salawati kepala burung block, west papua province, indonesia. Up to 1998, 160 exploration wells have been drilled in the basin.

Hydrocarbon in salawati basin is generated from tertiary and pretertiary source rock. By using the site, you must accept and abide by the terms and. Phillips, conoco, total and occidental subsequently tried to emulate trends success by exploring the adjacent bintuni basin, but found only. The biak basin and its setting in the birds head region. Job pertamina petrochina salawati boosts oil production in. Reactivation and production optimisation of teluk berau a. The terms and conditions set out below terms and conditions govern your use of the. Pant, institute of himalayan environment 3himalayan. Identification of fractured basement reservoir in swo field, salawati basin, west papua, based on seismic data. Directorate general of hydrocarbon 1 saurashtra basin. It was discovered in 1975 and had been producing since 2006. Explanatory notes for the energyresources map of the circum. Berita sedimentologi a sedimentological journal of the indonesia sedimentologists forum fosi, a commission of the indonesian association of geologist iagi from the editor.

Study of cambay and krishnagodavari basin for shale oil. Pdf identification of fractured basement reservoir in. Pdf noble et al 2016 kofiau and cendrawasih bay frontier. The spatial analysis of satluj basin, himachal pradesh rohit chauhan 1, jagdish chandra kuniyal 1department of geography, kumaun 2g. Directorate general of hydrocarbon saurashtra basin 1 basic introduction geographic location of the basin saurashtra basin is located in the northern part of western continental margin of india which. The field was discovered in 1970 and has produced nearly 600 mmbo and 1. The salawati basin, eastern indonesia, is an eastwest trending asymmetric foreland basin located on the northern margin of the indoaustralian continental plate. Development of the sorong fault zone north of misool.

Ob pertaminapetrochina salawati is 50 percent owned by pt pertamina hulu energi salawati, 16. The cambay basin in gujarat is the largest basin in the country, spreaded across 20,000 gross square miles, with a prospective area of 1940 square miles. Anambra basin is one of the energyrich inland sedimentary basins in nigeria 153 it is a nearly triangular shaped embayment covering about 3000 km 2 with a total sedimentary thickness of approximately 9. Review of water governance in the narmada river basin. Potential of prekais formation as a source rock in the. Salawati basin, eastern indonesia underwent tectonic reversal during the miocenepliocene as a response to the advent of the sorong fault megashear. The salawati basin, birds head of irian jaya, has been extensively explored. United states department of the interior geological survey undiscovered petroleum resources of indonesia by john kingston openfile report 88379 this report is preliminary and has.

The basin is located in the western part of birds head which hosts other sedimentary basins. Since 1936, salawati basin has produced more than 400 mmbo and 200 bcfg through 2014 1. Matugu unrisked net lundin potential recoverable resources mid case 9 mmboe salawati islandbasin 2007 exploration programme. The success of the program was the result of a combination of exploration techniques, including. Table 1 summarizes the inventory results sequentially by site id number for the samish. The rationale of the book is that knowledge of the basic principles of. Review of water governance in the narmada river basin 2 apart from this there are some granite, and the gondwana shale and sedimentary rocks in parts of the hills and plains and alluvial deposits near the. Evidences of multiple phases of basin inversion in narmada. The attaka field is located within the kutei basin, offshore east kalimantan, indonesia figure 1. Continent ocean interactions within east asian marginal seas, geophysical. During this period, the tilting of the basin rotated clockwisely from tilting southward, through. Studies pertaining to heat flow density distribution in indonesian tertiary sedimentary basins have been conducted intermittently throughout more than two decades. Pdf indonesian petroleum systems, reserve additions and.

Thermal modeling and heat flow density interpretation of. Basin analysis is an uptodate overview of the essential processes of the formation and evolution of sedimentary basins, and their implications for the development of hydrocarbon resources. But it is successful in small scale and difficult exploration, so a new exploration concept is needed to. Schematic diagram showing concept of basin formation by volcanic arc loading. Implication for structural evolution on salawati basin, seram and. Pdf basin formation by volcanic arc loading researchgate. Possible source rocks in the salawati basin include the klasafet and. Salawati basin sedimentary basin petroleum reservoir. Pdf on oct 1, 1995, james howes and others published indonesian. The data selection and validation process for the mekong river basin study involved three steps. The final sequence is marked by an unconformity caused by diachronous regional subsidence across the northern birds head that led to the drowning of localised carbonate platforms, including the.