The kabul basin covers an area of around 1600 km2 and is divided up into three subbasins. Salawati basin is a foreland basin located at the frontal edge of the indianaustralian continental plate. Development of the sorong fault zone north of misool. Smith bp research centre, sunbury on thames tw16 7ln, uk and b.
Its area is 1,623 km salawati is separated from new guinea to the southeast by the sele strait a. Carbonate drowning successions of the birds head, indonesia. In this basin, a number of petroleum systems can be recognized, each with associated subsystems. Accommodation is the interplay of eustatic sealevel changes, basin subsidenceuplift, local patterns of faulting.
The middle megasequence within the basin is composed of lower miocene platform carbonates possibly correlative with the kais limestone found in the salawati basin to the west. Ranking of indonesia sedimentary basin and storage capacity. Ghadames berkine basin, bounded on the north by the talemzanegefara arch, on the east by the hamra basin, on the south by the illizi basin, and on the west by the amguidhassi touareg structural axis. Pdf petroleum system cekungan salawati free download pdf. Seismic interpretation and depositional model of kaislower. Salawati basin, about 60 kilometres south of sorong. Around 20 tcf of gas has been classified as recoverable in this basin. Pdf identification of fractured basement reservoir in swo. Tanezzuftghadames structuralstratigraphic assessment unit. Tanezzuftghadames structuralstratigraphic assessment unit 20540301 triasghadames basin geologic province 2054 5 10 35 30 algeria tunisia libya m e d ite rra n e a n s e a sfax 0 250 500kilometers tanezzuftghadames structuralstratigraphic assessment unit 20540301 2056. But it is successful in small scale and difficult exploration, so a new exploration concept is needed to.
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. Figure 10 klasaman within petroleum system events chart of the salawati basin. Cenozoic plate tectonics and basin evolution in indonesia. 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. Description download petroleum system cekungan salawati comments.
Salawat on prophet muhammad sallallahu alayhi wasallam. Depositional environment of kg basin, east coast of india. Download as pptx, pdf, txt or read online from scribd. Development of the sorong fault zone north of misool, eastern. Pdf on jan 1, 2018, edy sunardi and others published facies and sequence stratigraphy. Papers cenozoic plate tectonics and basin evolution in indonesia m. 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 trends nnwsse. Report petroleum system cekungan salawati please fill this form, we will try to respond as soon as possible. Another important difference is the development of a 3 to 4kmdeep foreland basin adjacent to the irian jaya fold belt, which decreases to.
A guide to image interpretation, this book contains detailed color plates and tables that compare satellite imaging systems, list remote sensing web sites. Alternating thin versus thickskinned decollements, example. Siwaliks and oild bearing tertiary deposits free download as powerpoint presentation. A guide to image interpretation, this book contains detailed color plates and tables that compare satellite imaging systems, list remote sensing web sites, and detail photointerpretation equipment. The relatively undeformed australian continental plate in the south, with precambrian basement and relatively thin young sediment cover that is thickening into a foreland basin south of the central range. Geological setting of the salawati basin that controlled by left lateral sorong fault and nnessw. The seismic features of the reef carbonates in these two areas include chaotic bedding, intermittent internal reflections, chaotic or blank reflections, mounded reflections, and apparent amplitude anomalies, similar to the seismic characteristics of the lh111 reef reservoir in the dongsha uplift and island reef of the salawati basin, indonesia. The salawati basin was an active deep more than 4 km basin in geometric relation with the sorong fault. Study of cambay and krishnagodavari basin for shale oil. Siwaliks and oild bearing tertiary deposits sandstone. Pdf the salawati basin of western new guinea and the tomori basin of.
Pdf facies and sequence stratigraphy analyses of klasaman. Pdf identification of fractured basement reservoir in. Hydrocarbon in salawati basin is generated from tertiary and pretertiary source rock. Miocene reefs, east natuna basin 186 drapes, east natuna basin 187 salawati miocene reefs, salawatlbintuni basin 188 bintuni miocene reefs, salawatlbintun. Pdf the salawati basin of western new guinea and the tomori basin of eastern sulawesi, indonesia, are two sedimentary basins located either side of. Kais formation of the salawati basin located in the southeast part of the study area.
Implication for structural evolution on salawati basin, seram and. Salawati island psc h3 job pertaminabumi siak pusako j3 coastal plains pekanbaru psc b2 j4 j5 j6 j7 j8 j9 k1 k2 k3 k4 k5 k6 k7 k8 k9 sabang lamren banda aceh meulaboh langsa belawan medan kabu lhokseumawe bagansiapiapi sibolga dumai pekanbaru rengat dabo batam tanjung pinang jambi bengkulu palembang. Correlation of the salawati and tomori basins, eastern. Galowa strait, revenges strait, and from batanta to the north by the pitt strait a. As a partner in our projects and construction practice, merrick advises clients on all aspects of energyrelated development projects and transactions, from the granting of upstream concession agreements to the acquisition and disposal of energy assets. Bibliography of indonesia geology and surrounding areas. Basin 189 miocene drapes, salawati bintuni basin 190. Hydrocarbon potential of eastern indonesia and required. Pdf correlation of the salawati and tomori basins, eastern. At this point, the total score of basin suitability has been resulted. Pdf unravel structural evolution through palinspastic. The klasafet formation has been assumed as the main hydrocarbon source rock in salawati basin deposited in the shallow marine environment during middle miocene time. Miocene drapes, salawati bintuni basin 190 cretaceous drapes, salawatlbintuni basin 191 neogene folded sandstones salwatlbintuni basin 192 salawatlpilocene diapirs, salawati. Seismic characteristics of a reef carbonate reservoir and.
The krishnagodavari basin is located in the southeastern part of the godavari valley, trending nesw and cretaceous successions comprising raghavapuram early cretaceous. The onland part of the basin is also known as saurashtra peninsula. The movement of sfz involves rotation and translation that separates salawati basin from the birds head region with basement high as the boundary of the basin. Structure and hydrocarbon potential of the new guinea fold. Source rocks study and thermal modelling in salawati basin, west. To the end, in order to see which basin position on the top ten rank, basin score are sorted descending.
The salawati basin is recognized as the one of big prolific oil basin in eastern indonesia with a total cumulative oil production more than 300 million barrel oil. During 2017, the gross production of the onshore fields was 61,827 barrels of oil. Salawati island psc h3 job pertaminabumi siak pusako j3 coastal plains pekanbaru psc b2 j4 j5 j6 j7 j8 j9 k1 k2 k3 k4 k5 k6 k7 k8 k9 sabang lamren banda aceh meulaboh langsa belawan medan kabu lhokseumawe bagansiapiapi sibolga dumai pekanbaru rengat dabo batam tanjung pinang jambi bengkulu palembang pangkalpinang. Sorong fault, a major strikeslip fault in eastern indonesia and terminating the basin to the north, has inverted the basin s polarity in the. Sediment supply is a function of climate exerting controls on.
Merrick white specialises in global oil, gas, lng, refining and petrochemical project development. Tanezzuftghadames structuralstratigraphic assessment. Pdf structural evolution of salawati basin is analyzed based on palinspastic reconstructions of interpreted seismic reflection data to unravel the. Since 1936, salawati basin has produced more than 400 mmbo and 200 bcfg through 2014 1.
In the onshore kutei basin, largely comprising inverted synrift sequences where as yet few hydrocarbons have been located, howes and tisnawijaya 1995 suggested that an early synrift to early postrift petroleum system, the tanjung berai. Selected geologic characteristics pertinent to occurrence of producible oil and gas resources are also shown when available. The tangguh gas field is a gas field lies in bintuni bay, in the province of west papua, indonesia. I will try to follow syntax of qbasic as close as i can.
I am developing this interpreter for selflearning purposes,dont take it serious. Salawati is one of the four major islands in the raja ampat islands in west papua formerly irian jaya, indonesia. The salawati basin of northwestern irian jaya a broad zone of regional leftlateral shear usually indonesian western new guinea is the most known as the sorong fault zone figs 1 2. Pdf development of the sorong fault zone north of misool. The following maps show the drilling history and oil and gas production of selected lowpermeability, continuoustype shale reservoirs. Allah and his angels send blessings on the prophet. More than 200 seismic lines have been interpreted in the seram, misool, and salawati offshore. Oil and gas exploration, resources, and production.
United states department of the interior geological survey undiscovered petroleum resources of indonesia. The major source rocks are the silurian tanezzuft formation and middle to upper devonian mudstone. Seismic characteristics of a reef carbonate reservoir and implications for hydrocarbon exploration in deepwater of the qiongdongnan basin, northern south china sea. Secara geografis kawasan timor basin berada di sekitar koordinat 8034 ls. Purchase of an open document does not constitute license for republication in any form, nor does it allow web posting without prior written permission. The top is marked by a lower miocene angular unconformity that can be traced to basins in the bintuni region to the west. You can search for and view abstracts or first pages if digital abstract not available for individual papers.
Study of cambay and krishnagodavari basin for shale oil and gas. The deformed zone of the leftlateral sorong fault separates the basin with the. But it is successful in small scale and difficult exploration, so a new exploration concept is. Reservoirs inwalio area of kepala burung psc, salawati basin, west. Class j 1 j2 j3 j4 j5 weight on offshore 1 4 10 0,15 geothermal 1 3 7 0, geology 1 3 7 0,11 tectonic setting 1 8 10 15 0,09. Pkf4 resembles a thermal subsidence unit which onlaps pkf3 and is truncated by kf1. The basin extends southeast into the deep waters of the bay of bengal. Directorate general of hydrocarbon 1 saurashtra basin. This searchable database comprises the full ipa publications archive comprising ipa convention proceedings from 1972 to the presentday, technical symposiums and other special publications. Southwest of the eastern papuan fold belt, there is no foreland basin, and the top of the miocene limestone is currently at sea level. Potential of prekais formation as a source rock in the salawati basin, bird head, west papua, indonesia pireno, gadjah e. A significant part of the onshore basinal area is covered by quaternary alluviam.
The salawati basin here is made up of three prominent structural and depositional elements, namely a shallow shelf which adjoins the ayamaru high on the east and south, an area conducive to prolific reef development, and a deep trough exten ding to the sorong fault zone into which a thick sec tion of pleistocene clastics accumulated. In eastern indonesia only the salawati basin is considered to be mature. Salawati basin sedimentary basin petroleum reservoir. Kofiau basin fill the kofiau basin fill sequence is subdivided into two parts kf1 and kf2 which appear to have been deposited in part during an interval of rapid subsidence. It is estimated that the krishna godavari basin, located in eastern india, holds the largest shale gas reserves in the.
The natural gas field contains over 500 billion cubic metres 18 trillion cubic feet of proven natural gas reserves, with estimates of potential reserves reaching over 800 billion cubic metres 28 trillion cubic feet the tangguh field is developed by a consortium of international. Though they may differ slightly in age and development, they share many characteristics. Salawati is separated from new guinea to the southeast by the sele strait a. Ranking of indonesia sedimentary basin and storage. The salawati basin, eastern indonesia, is an eastwest trending asymmetric foreland basin located on the northern margin of the indoaustralian continental plate. Potential of prekais formation as a source rock in the. Geology and hydrogeology of the kabul basin iii s u m m a r y the kabul basin is a plateau surrounded by mountains located in the eastern central part of the country, and is the site of the afghan capital. Solve every difficulty problem affliction in your life by reciting salawat on prophet sallallahu alayhi wasallam.
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