The basin is presently bounded to the north by the sorong fault zone which separates the australian continental plate to the south from the pacific oceanic plate to. It consists predominantly of a gently undulating plain with an average elevation varying from 250 to 400. 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. Introduction he geology of the majalengka subbasin has been studied by many researchers since the last decades of the 19th century. Evidences of multiple phases of basin inversion in narmada. Pkf4 resembles a thermal subsidence unit which onlaps pkf3 and is truncated by kf1. Pdf identification of fractured basement reservoir in.
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. Seismic interpretation and depositional model of kaislower. Lastly mandawa basin which categorized into groups and formation. Sedimentary controls on the sequence stratigraphic architecture in intracratonic basins. Purchase of an open document does not constitute license for republication in any form, nor does it allow web posting without prior written permission. Selected geologic characteristics pertinent to occurrence of producible oil and gas resources are also shown when available. An example from the lower permian shanxi formation, ordos basin, northern china author links open overlay panel hongtao zhu a b keyu liu c d xianghua yang a b qianghu liu a b. The iullemmeden basin in northwestern nigeria is known locally as the sokoto basin. Attribute analysis in a 3d seismic area of kerala deepwater basin a case study. Keywordspetroleum system, kerogen type iii, rockeval pyrolysis, sediment turbidite i. Type your address into the search bar and press enter. A gisbased approach in drainage morphometric analysis of kanhar river basin, india praveen kumar rai kshitij mohan sameer mishra aariz ahmad varun narayan mishra received.
Apr 30, 2009 the iullemmeden basin in northwestern nigeria is known locally as the sokoto basin. It overlies the granitic basement of eastern dharwar craton with a profound unconformity and has faulted contacts at many places. Each cavern can produce halite about 201,901 tons, considered the purity of rock salt 97%. Potential of prekais formation as a source rock in the. The deformed zone of the leftlateral sorong fault separates the basin with the. Bhima basin the ne trending irregularly sinous bhima basin fig. The sokoto basin nigerian sector of the iullemmeden basin. Stratigraphic evolution of oligocenemiocene carbonates and. Sirhanturayf basin of northwestern saudi arabia fig. Review article tectonic framework and evolutionary. Arcims viewer legend layers overview map view entire state previous view clear selection search create pdf. The interval of study is the klasaman formation that is characterized by thick sediment intercalated sandstones and shales.
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. The elongation ratio of the chalakudi basin is estimated as 0. This study is very important to give a contribution for developing exploration prospect by predicting. Preliminary geologic map of the wadi as sirhan quadrangle. The spatial analysis of satluj basin, himachal pradesh, india. Geoenvironmental assessment of loni nala subunit, gomati basin, india, using gis technique archana gupta1, biswajeet thakur2, akanksha shukla1 and dhruv sen singh3 1 department of geography, university of lucknow, lucknow226007 2 birbal sahni institute of palaeobotany, lucknow226007. Pdf on jan 1, 2018, edy sunardi and others published facies and. Like its immediate neighboring, krishnagodavari basin, mahanadi basin also has a geological extension into offshore. Tectonic framework and evolutionary history of the bengal basin in the indian subcontinent a. A layered block called a graben has dropped down in the middle relative to the blocks on either side of the. Facies and sequence stratigraphy analyses of klasaman. This study incorporates outcrop and subsurface data of. Tapi basin basin description geographical description the tapi is the second largest westward draining interstate river basin.
The anambra basin is situated west of the lower benue trough and is often considered youngest formation of the benue trough. It consists predominantly of a gently undulating plain with an average elevation varying from 250 to 400 m above sealevel. Pacet septic tank site on the bank of the citarum river at desa rancamanyar, kec. The krishnagodavari basin is located in the southeastern part of the godavari valley, trending nesw and cretaceous successions comprising raghavapuram early cretaceous. Estimated crude oil production in 2002 was 2540 and 10,676 bblday from cepu and tuban blocks, respectively petroleum report of indonesia, 20022003, american embassy jakarta, 2004. Download the latest version of adobe reader, free of charge. A case study of sukhna lake watershed in lower shiwalik, india.
Reservoirs inwalio area of kepala burung psc, salawati basin, west. Stratigraphic modelling has been increasingly used to assist stratigraphic interpretation and basin analysis, particularly in the field of petroleum exploration. The spatial analysis of satluj basin, himachal pradesh rohit chauhan 1, jagdish chandra kuniyal 1department of geography, kumaun 2g. The drainage density of the basin is estimated as 2. 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. Development of the sorong fault zone north of misool.
Morphometric analysis of drainage basin through gis. Click anywhere on the map and the feature will appear. Implication of drainage basin parameters of a tropical river. Upper citarum river basin, kampung jirihieun, desa pangauban, kec. Introduction he geology of the majalengka subbasin has been studied by many. Estimation of flow for u ngauged watersheds in pranhita of. Correlation of the salawati and tomori basins, eastern. Implication of drainage basin parameters of a tropical. Pant, institute of himalayan environment 3himalayan. It extends northwestward into the niger valley, northward to the jos massif and northeastward into lafia. Zoom in zoom out pan rect identify select object buffer distance.
Review of water governance in the narmada river basin. Attribute analysis in a 3d seismic area of kerala deepwater. Depositional environment of kg basin, east coast of india. Rainfall 1n this basin is mainly due to southwest monsoon current and its distribution is influenced by physical features. The sirhanturayf basin is a shallow sedimentary basin that extends north and west into iraq and jordan. The basin is bounded to the south by the niger delta basin hinge line. Structural and depositional evolution, kh field, west natuna basin, offshore indonesia. The ideas proposed below are not critically dependent on this proposed age or the synchronicity of basin formation. Kasim and walio fieldsindonesia salawati basin, irian jaya. Geology and tectonic evolution of bird head region papua.
But it is successful in small scale and difficult exploration, so a new exploration concept is needed to. Roy1, and alokesh chatterjee2 1department of geology, presidency university, kolkata 700 073, india. Geoenvironmental assessment of loni nala subunit, gomati basin, india, using gis technique archana gupta1, biswajeet thakur2, akanksha shukla1 and dhruv sen singh3. More than 200 seismic lines have been interpreted in the seram, misool, and salawati offshore. 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 river courses.
Estimated crude oil production in 2002 was 2540 and 10,676 bblday from cepu and tuban blocks, respectively pe. Identification of fractured basement reservoir in swo field, salawati basin, west papua, based on seismic data. This test encountered a highly porous miocene limestone containing. Noble et al 2016 kofiau and cendrawasih bay frontier basin. Natuna area, pliocene and miocene hydrocarbon identification view project. 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. The biak basin and its setting in the birds head region.
Miocene drapes, salawati bintuni basin 190 cretaceous drapes, salawatlbintuni basin 191 neogene folded sandstones salwatlbintuni basin 192 salawatlpilocene diapirs, salawati. The results of their studies were summarized and well documented by 1. Implication of drainage basin parameters of a tropical river basin of south india. Aqueduct metadata document mekong river basin study pdf. The basin extends southeast into the deep waters of the bay of bengal. Roy1, and alokesh chatterjee2 1department of geology, presidency university, kolkata 700 073, india 2hoogli moshin college, hoogli 712 101, india the bengal basin evolved as a riftcontrolled extensional basin along the nnessw trending basin mar. Pdf identification of fractured basement reservoir in swo. Accommodation is the interplay of eustatic sealevel changes, basin subsidenceuplift, local patterns of faulting. Reinterpretation of the sembakung oilfield, kalimantan, indonesia utilizing modern 3d seismic data tony edwards equatorial energy international inc. The data selection and validation process for the mekong river basin study involved three steps. Kais formation of the salawati basin located in the southeast part of the study area.
Salawati basin sedimentary basin petroleum reservoir. It occupies parts of jagdalpur district of chhattisgarh and koraput district of orissa and rests nonconformably on the archaean. Estimation of flow for u ngauged watersheds in pranhita of godavari river basin in india using swat. Carbonate drowning successions of the birds head, indonesia. Basins and major watersheds in minnesota basins cedar river des moines river lake superior lower mississippi river minnesota river missouri river rainy river red river of the north st. Northern salawati basin, papua, indonesia find, read and cite all the. 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. A gisbased approach in drainage morphometric analysis of. Hydrocarbon in salawati basin is generated from tertiary and pretertiary source rock.
Pdf facies and sequence stratigraphy analyses of klasaman. P 368 evidences of multiple phases of basin inversion in narmada block, south cambay basin, gujarat, india rajeev mohan 1, s. After solutioning is complete, there will be halite. Land, water and soil are limited natural resources and their widely utilizationwith increased population is a major concern. Rufiji river as the boundary between mandawa basin and ruvu basin.
Pdf documents opened from your browser may not display or print as intended. 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. Source rocks study and thermal modelling in salawati basin, west. Reinterpretation of the sembakung oilfield, kalimantan. Saltreservekhorat basin solution miningdesign the objective of this research is to compute the salt reserve estimation for the lower salt member in the khorat basin. Since 1936, salawati basin has produced more than 400 mmbo and 200 bcfg through 2014 1. 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. The following maps show the drilling history and oil and gas production of selected lowpermeability, continuoustype shale reservoirs. Geological survey editorial standards and stratigraphic nomenclature 1988.
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. Panda summary search for hydrocarbon in a sparsely explored basin is mainly driven by seismic methods. Two major oil and gas producing basins were discovered in the region namely the salawati and bintuni basins. E, petrizzo mr 2007 practical manual of neogene planktonic foraminifera. 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. Sedimentary controls on the sequence stratigraphic. The salawati basin, eastern indonesia, is an eastwest trending asymmetric foreland basin located on the northern margin of the indoaustralian continental plate. Review article tectonic framework and evolutionary history of. For best results viewing and printing pdf documents, it is recommended that you download the documents to your computer and open them with adobe reader.
A new challenge and opportunity for hydrocarbon exploration in pretertiary basement. Understanding basin development requires a better knowledge of the mesozoic and early cenozoic history of sundaland, which mainly lacks rocks of this age. 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. Development of the sorong fault zone north of misool, eastern. More than 200 seismic lines have been interpreted in the seram, misool, and salawati. Synopsis of water resources of the ipswich river basin. The x well is located in the salawati basin which is part of western papua. The high basin relief indicates high runoff and sediment transport. This article is published with open access at abstract the study indicates that. United states department of the interior geological survey undiscovered petroleum resources of indonesia. Basin introduction the mahanadi basin, a product of rifting and break up of gondwana land, situated on the east coast of india figs.
The texas watershed viewer allows users to identify local watersheds, sub watersheds, river basins, and river sub basins throughout the state of texas. Sediment supply is a function of climate exerting controls on. Humid zones are found only in the west on the hills. Oil and gas exploration, resources, and production. The movement of sorong fault strongly controlled the sedimentation of this formation. View the article online for updates and enhancements.
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