Salawati is one of the four major islands in the raja ampat islands in west papua formerly irian jaya, indonesia. Pdf identification of fractured basement reservoir in swo. Aqueduct metadata document mekong river basin study. Part or all of this report is presented in portable document format pdf. White abstract the part of sorong fault zone studied here is located to the. Pdf the salawati basin of western new guinea and the tomori basin of. Revus 30%, rwedea 20% unrisked net lundin potential recoverable resources mid case 125 mmboe pl338. A new challenge and opportunity for hydrocarbon exploration in pretertiary basement. Implemented in the advanced weather interactive processing system awips, ffmp is used to assist in flash flood warning decisions at 121 weather forecast offices wfos throughout the country. 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. Synopsis of water resources of the ipswich river basin. Even so, all of these studies have always concentrated on the basic compilations of thermal gradient, thermal conductivity, and terrestrial heat flow datasets or the study of basin thermal history rather than on the investigations. The x well is located in the salawati basin which is part of the western birds head of papua island.
Development of the sorong fault zone north of misool, eastern. 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. Pdf identification of fractured basement reservoir in. Sediment supply is a function of climate exerting controls on.
This formation is laterally equivalent to the klamogun limestone of salawati basin. Zonation conservation rankings based on species distribution models for 198 land bird species under current 19712000 climate conditions. 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. Seismic interpretation and depositional model of kaislower. I will try to follow syntax of qbasic as close as i can. This search has been lack in the pursuit of new petroleum system in the of. Selected geologic characteristics pertinent to occurrence of producible oil and gas resources are also shown when available. Selected geologic characteristics pertinent to occurrence of. The biak basin and its setting in the birds head region of west.
Secara geografis kawasan timor basin berada di sekitar koordinat 8034 ls. Since some new system files are included in this release, you may need to restart windows after some files have been updated before continuing with the installation. The fault zone cuts an early miocene collision suture between the philippine sea plate and the northern australian margin. 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. Geological survey editorial standards and stratigraphic nomenclature 1988. Salawati basin sedimentary basin petroleum reservoir. Studies pertaining to heat flow density distribution in indonesian tertiary sedimentary basins have been conducted intermittently throughout more than two decades.
The evidence of divergence and horsetail structure at nw birds head and salawati basin, west papua, indonesia putri riadini1 and benyamin sapiie2. The salawati basin records the reversal of basin with that at the kaisklasafet level satyana et al. I am developing this interpreter for selflearning purposes,dont take it serious. In addition, in the salawati and bintuni basins the kais formation partly interfingers and is conformably overlain by the klasafet formation dow et al, 1988.
Transforming river basin management indiaenvironmentportal. Though they may differ slightly in age and development, they share many characteristics. Thermal modeling and heat flow density interpretation of the. The quality of the nile waters has generally deteriorated because of population growth, intensification of agriculture, and industrial development. Reservoirs inwalio area of kepala burung psc, salawati basin, west. It is the fifth largest river in the country and the. The water resources of the nile basin nile basin initiative. This study is very important to give a contribution for developing exploration prospect by predicting. The following national map portrays the location of fields identified as being among. Irian jaya is the easternmost province of indonesia and is located on the western half of the island of new guinea. Download this full collection of wash basin 3d cad blocks cad models. Synopsis of water resources of the ipswich river basin, massachusetts. The following maps show the drilling history and oil and gas production of selected lowpermeability, continuoustype shale reservoirs. This 5day course covers the key aspects of basin analysis.
Oil and gas exploration, resources, and production. Thermal modeling and heat flow density interpretation of. Geological setting of the salawati basin that controlled by leftlateral sorong fault and nnessw. Transforming river basin management stories from the koshi basin. Facies and sequence stratigraphy analyses of klasaman. Groundwater is the dominant source of domestic water supply in rural communities across the basin. White abstract the part of sorong fault zone studied here is located to the north of misool between obi and batanta. The knownhydrocarbonreservoirs are the mesozoic sandstones, particularly the toro sandstone in png. A gisbased approach in drainage morphometric analysis of. 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.
Map of salawati blntunl basin showing areas of plays, trends, and significant tests 126 67. The utilisation of narmada river basin today is hardly about 10%. The sokoto basin nigerian sector of the iullemmeden basin. United states department of the interior geological survey undiscovered petroleum resources of indonesia by john kingston open file report 88379 this report is preliminary and has. Morphotectonics of the jamini river basin, bundelkhand. The narmada, the largest west flowing river of the peninsula, rises near amarkantak range of mountains in madhya pradesh. Salawati is separated from new guinea to the southeast by the sele strait a.
This cad drawing comprises a variety of interior design models. The interval of study is the klasaman formation that is characterized by thick sediment intercalated sandstones and shales. This searchable database comprises the full ipa publications archive comprising ipa convention proceedings from 1972 to the presentday, technical symposiums. The governments of afghanistan, australia, austria, bangladesh, bhutan. Pdf documents opened from your browser may not display or print as intended. Hydrocarbon in salawati basin is generated from tertiary and pretertiary source rock.
Furthermore, the region is developing rapidly on the economic front, and a major part of this rapid development is built on natural resources. Facies and sequence stratigraphy analyses of klasaman formation. 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. The movement of sorong fault strongly controlled the sedimentation of this formation. The geology of indonesiapapua wikibooks, open books for. It is a region that must be understood if we are to understand mountain belts, arc development, marginal basin evolution and, more generally, the behaviour of the lithosphere in collision settings. 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. Development of the sorong fault zone north of misool. Source rocks study and thermal modelling in salawati basin, west. The natural gas field contains over 500 billion cubic metres 18 trillion cubic feet of proven natural gas. Its area is 1,623 km salawati is separated from new guinea to the southeast by the sele strait a.
The tangguh gas field is a gas field lies in bintuni bay, in the province of west papua, indonesia. Accommodation is the interplay of eustatic sealevel changes, basin subsidenceuplift, local patterns of faulting. One of potential reservoir rocks in this basin is the coarse siliciclastic of early pliocene klasaman formation 1 2. Elements of basin analysis basin analysis basin analysis is a process that requires the. Zonation is a spatial conservation planning software tool that can take into account multiple species to create a hierarchical prioritization of the landscape.
The island of new guinea is the second largest island in the world and includes puncak jaya 4884 m, the highest peak in southeast asia and australia. Another important difference is the development of a 3 to 4kmdeep foreland basin adjacent to the irian jaya fold belt, which decreases to. The geology of indonesiapapua wikibooks, open books for an. Stratigraphy, facies, and diagenesis of limestone in wurui. Download the latest version of adobe reader, free of charge. Pdf facies and sequence stratigraphy analyses of klasaman.
Current zonation prioritization for california land birds. Managing ecosystems, transforming landscapes, creating buffers 2 understanding the tana basin 2. Development of the sorong fault zone north of misool eastern indonesia afif saputra robert hall lloyd t. This project involves the delineation of flashfloodscale basins for use in the nws ffmp system. Basins download and installation environmental modeling.
Structure and hydrocarbon potential of the new guinea fold. In the salawati basin and the gulf of papua, oil and gas are trapped in miocene reefs figure 1. This basin is one of the major hydrocarbon regions in indonesia. It consists predominantly of a gently undulating plain with an average elevation varying from 250 to 400. This searchable database comprises the full ipa publications archive comprising ipa convention proceedings from 1972 to the presentday, technical symposiums and other special publications. 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. Pdf correlation of the salawati and tomori basins, eastern. Tectonic evolution of southeast asia robert hall, derek. Directorate general of hydrocarbon 1 saurashtra basin. The upper shoreface sandstones of parasequence4 to 9 can be potential reservoir rocks in the. Wash basin 3d cad models cad design free cad blocks.
The main hydrocarbon source rocks are in distal jurassic and possibly cretaceous shales. Morphotectonics of the jamini river basin, bundelkhand craton. Sedimentary controls on the sequence stratigraphic. Implemented in the advanced weather interactive processing system awips, ffmp. Lack of knowledge in characteristics and thermal modelling source rock in sirga and prefaumai formation. The data selection and validation process for the mekong river basin study involved three steps. The iullemmeden basin in northwestern nigeria is known locally as the sokoto basin. 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. 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 annual run of the dam site at 75 percentage of dependability is 27. The research area is located about 100150 km east of salawati basin and bintuni. The kabul basin covers an area of around 1600 km2 and is divided up into three subbasins. 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. Identification of fractured basement reservoir in swo field, salawati basin, west papua, based on seismic data. The x well is located in the salawati basin which is part of western papua. Galowa strait, revenges strait, and from batanta to the north by the pitt strait a. Gradual sediment accumulation of the basin gives rise to a backstepping or retrogradational sequence due to the increase of relative accommodation space by sediment including associated water infill thereby causing the base level to elevate accordingly e. Pdf on jan 1, 2018, edy sunardi and others published facies and sequence stratigraphy. Sep 22, 2016 studies pertaining to heat flow density distribution in indonesian tertiary sedimentary basins have been conducted intermittently throughout more than two decades. These basins have been proven to produce oil and gas.
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