Canning Basin (original) (raw)
Canning Basin – basen sedymentacyjny, położony w Australii Zachodniej. Canning Basin zajmuje obszar około 506 000 km², z czego 430 000 km² położona jest na ladzie. Na tym obszarze znajdują się złoża ropy i gazu, w czerwcu 2003 roku wykonano 250 studni. Basen jest odrębnym rejonem fizjograficznym .
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| dbo:abstract | Das Canningbecken ist ein Sedimentbecken in Western Australia. Das Becken erstreckt sich über 506.000 km², von denen 430.000 km² auf dem Festland liegen. Die restliche Fläche befindet sich offshore. Das Sedimentationsbecken hat teilweise eine Mächtigkeit von 15 km. Es besteht aus Sedimenten, die sich in großen Depots ablagerten. Das nördlichste ist der Fitzroy Trough-Gregory Sub-basin complex und die südlichsten sind der Willara-Sub-basin- und Kidson Sub-basin complex. Der Fitzroy-Komplex läuft offshore weiter. Das Canningbecken durchlief in seiner Entstehung mehrere Phasen. Im Devon entstand im Canningbecken das so genannte „devonische Great-Barrier-Riff“, ein großes System von Tabulaten-Stromatoporen-Riffen mit einer ursprünglichen Länge von wahrscheinlich mehr als 1.000 Kilometern. Im Canningbecken waren die Bedingungen für die Bildung dieses riesigen Riffkomplexes optimal, da das Gebiet im Devon in der Nähe des Äquators lag und von einem flachen, tropischen Meer bedeckt war. Im Mai 1981 wurde das Blina-Ölfeld gefunden, das 105 km südöstlich der Stadt Derby liegt. Es war die erste wirtschaftlich verwertbare Ölquelle im Canningbecken. Das Öl befand sich in der Nullara Limestone Formation (Nullar Oil Pool) und in der Lower Carboniferous dolomitic Yellow Drum Formation (Yellow Drum Oil Pool). Unweit davon wurde ein weiteres Ölfeld gefunden, das Backreef-1. Das große Sedimentbecken wurde auf 78.000 km Länge durch seismologische Sprengungen untersucht und es wurden insgesamt 250 Brunnen gebohrt. (de) The Canning Basin is a geological basin located in Western Australia. Deposition of sediments began after early-Ordovician thermal subsidnce, and continued into the Early Cretaceous. The Basin covers approximately 506,000 km2 of which approximately 430,000 km2 is on land. It has been recognised as having prospective oil and gas capacity and has been studied extensively; as of June 2003 250 wells have been drilled and 78,000 km of seismic shot. The basin is also a distinct physiographic province of the larger West Australian Shield division. The Canning Basin is home to a Devonian fossil reef complex that stretches 350 km across the northern edge of the basin. The fossil reef is very well preserved and is cut by several modern canyons, including Geikie Gorge and Windjana Gorge.The fossil sites associated the ancient reef system that extended for around one thousand kilometres along what is now the northwest of the Australian continent, described as resembling the modern Great Barrier Reef off the coast of Eastern Australia. The sites have produced ancient fossil material in an excellent state of preservation, most notably those revealing details of the structure of skeletons and soft-tissues of early amphibians. One important site is referred to as the "Devonian 'Great Barrier Reef'", and another, the "Gogo fish fossil site" (the Gogo formation), is named for the discovery of the Gogo fish. The internal features of the basin include: * sub basins - the Fitzroy Trough-Gregory Sub-basin complex, the Willara Sub-basin, and the Kidson Sub-basin complex * shelves - Anketell shelf, Billiluna shelf, Tabletop shelf, Lennard shelf, Ryan Shelf * terraces - Balgo terrace The Australian Bureau of Mineral Resources report of the geology of the basin outlines the early exploration: The Bureau started field work in the Canning Basin in 1947 and continued every year up to 1958. This work was carried out by geological parties equipped with land vehicles (1947-56) and with a helicopter (1957), by seismic and gravity parties, by an airborne magnetic party, and by a stratigraphical drilling party (1955-58). All work was based on air photographs, at a scale of 1:50,000, prepared by the R.A.A.F. This bulletin incorporates the results of all these surveys. The first attempt at compiling a geology of the Canning Basin was made by Reeves in 1949 (en) Canning Basin – basen sedymentacyjny, położony w Australii Zachodniej. Canning Basin zajmuje obszar około 506 000 km², z czego 430 000 km² położona jest na ladzie. Na tym obszarze znajdują się złoża ropy i gazu, w czerwcu 2003 roku wykonano 250 studni. Basen jest odrębnym rejonem fizjograficznym . (pl) Canning Basin är en sänka i Australien. Den ligger i delstaten Western Australia, omkring 1 500 kilometer nordost om delstatshuvudstaden Perth. Omgivningarna runt Canning Basin är i huvudsak ett öppet busklandskap. Trakten runt Canning Basin är nära nog obefolkad, med mindre än två invånare per kvadratkilometer. Genomsnittlig årsnederbörd är 490 millimeter. Den regnigaste månaden är januari, med i genomsnitt 161 mm nederbörd, och den torraste är augusti, med 1 mm nederbörd. (sv) 坎宁盆地（英語：Canning Basin）亦译甘宁盆地，也称荒漠自流盆地（Desert Artesian Basin），是澳大利亚西澳大利亚州西北部一个干旱的沉积盆地，面积约40万平方公里，北起，南至，西抵印度洋海岸，东以东经128°为界，属于大沙沙漠西北部分。腹地多沙丘，间有黏土平地，有自流泉。因盆地下面有地壳下陷，多地震活动。富有石油和天然气资源，布利纳油田位于该地区。 (zh) |
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| rdfs:comment | Canning Basin – basen sedymentacyjny, położony w Australii Zachodniej. Canning Basin zajmuje obszar około 506 000 km², z czego 430 000 km² położona jest na ladzie. Na tym obszarze znajdują się złoża ropy i gazu, w czerwcu 2003 roku wykonano 250 studni. Basen jest odrębnym rejonem fizjograficznym . (pl) Canning Basin är en sänka i Australien. Den ligger i delstaten Western Australia, omkring 1 500 kilometer nordost om delstatshuvudstaden Perth. Omgivningarna runt Canning Basin är i huvudsak ett öppet busklandskap. Trakten runt Canning Basin är nära nog obefolkad, med mindre än två invånare per kvadratkilometer. Genomsnittlig årsnederbörd är 490 millimeter. Den regnigaste månaden är januari, med i genomsnitt 161 mm nederbörd, och den torraste är augusti, med 1 mm nederbörd. (sv) 坎宁盆地（英語：Canning Basin）亦译甘宁盆地，也称荒漠自流盆地（Desert Artesian Basin），是澳大利亚西澳大利亚州西北部一个干旱的沉积盆地，面积约40万平方公里，北起，南至，西抵印度洋海岸，东以东经128°为界，属于大沙沙漠西北部分。腹地多沙丘，间有黏土平地，有自流泉。因盆地下面有地壳下陷，多地震活动。富有石油和天然气资源，布利纳油田位于该地区。 (zh) Das Canningbecken ist ein Sedimentbecken in Western Australia. Das Becken erstreckt sich über 506.000 km², von denen 430.000 km² auf dem Festland liegen. Die restliche Fläche befindet sich offshore. Das Sedimentationsbecken hat teilweise eine Mächtigkeit von 15 km. Es besteht aus Sedimenten, die sich in großen Depots ablagerten. Das nördlichste ist der Fitzroy Trough-Gregory Sub-basin complex und die südlichsten sind der Willara-Sub-basin- und Kidson Sub-basin complex. Der Fitzroy-Komplex läuft offshore weiter. Das Canningbecken durchlief in seiner Entstehung mehrere Phasen. (de) The Canning Basin is a geological basin located in Western Australia. Deposition of sediments began after early-Ordovician thermal subsidnce, and continued into the Early Cretaceous. The Basin covers approximately 506,000 km2 of which approximately 430,000 km2 is on land. It has been recognised as having prospective oil and gas capacity and has been studied extensively; as of June 2003 250 wells have been drilled and 78,000 km of seismic shot. The basin is also a distinct physiographic province of the larger West Australian Shield division. The internal features of the basin include: (en) |
| rdfs:label | Canningbecken (de) Canning Basin (en) Canning Basin (pl) Canning Basin (sv) 坎宁盆地 (zh) |
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