Junggar Basin (original) (raw)
중가르 분지(중국어 간체자: 准噶尔, 정체자: 準噶爾, 병음: Zhǔngáěr)는 중화인민공화국 신장 위구르 자치구의 북부, 알타이 산맥과 톈산 산맥 사이에 끼여 있으며 동부는 해발 1,000m, 서부는 해발 500m이다. 이 문서에는 다음커뮤니케이션(현 카카오)에서 GFDL 또는 CC-SA 라이선스로 배포한 글로벌 세계대백과사전의 내용을 기초로 작성된 글이 포함되어 있습니다.
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| dbo:abstract | Džungarská pánev (ujgursky جۇڭغار ئويمانلىقى, Jungghar oymanliqi, čínsky 准噶尔盆地, Junggar Pendi, pinyin Zhǔngáěr Péndì, český přepis Čun-ka-er pchen-ti) je oblast na severozápadě Ujgurska a Čínské lidové republiky, mezi pohořími Altaj na severu, Ťan-šan na jihu a Tarbagataj (který se někdy považuje za součást Ťan-šanu) na západě. Nadmořská výška kolísá, místy překračuje i 1000 m, ale hladina jezera Ebinur v jihozápadním cípu pánve leží pouze 190 m n. m. Podstatnou část pánve vyplňuje druhá největší čínská poušť . Většina pánve je bez odtoku, pouze její severní částí protéká řeka Irtyš (Ertis Che). Po jižním okraji pánve vede důležitá silniční i železniční spojnice Číny s Kazachstánem. Leží tu i ujgurské hlavní město Urumči. Z něj vede silnice i železnice snadným průsmykem přes Ťan-šan k jihu do a dále do vlastní Číny. Naopak západní konec této trasy leží v Džungarské bráně, která spojuje Džungarskou pánev s Balchašsko-alakolskou pánví na území Kazachstánu. (cs) The Junggar Basin (simplified Chinese: 准噶尔盆地; traditional Chinese: 準噶爾盆地) is one of the largest sedimentary basins in Northwest China. It is located in Xinjiang, and enclosed by the Tarbagatai Mountains of Kazakhstan in the northwest, the Altai Mountains of Mongolia in the northeast, and the Heavenly Mountains (Tian Shan) in the south. The geology of Junggar Basin mainly consists of sedimentary rocks underlain by igneous and metamorphic basement rocks. The basement of the basin was largely formed during the development of the Pangea supercontinent during complex tectonic events from Precambrian to late Paleozoic time. The basin developed as a series of foreland basins – in other words, basins developing immediately in front of growing mountain ranges – from Permian time to the Quaternary period. The basin's preserved sedimentary records show that the climate during the Mesozoic era was marked by a transition from humid to arid conditions as monsoonal climatic effects waned. The Junggar basin is rich in geological resources (e.g. petroleum, coal and ore deposits) due to effects of volcanism and sedimentary deposition. (en) 중가르 분지(중국어 간체자: 准噶尔, 정체자: 準噶爾, 병음: Zhǔngáěr)는 중화인민공화국 신장 위구르 자치구의 북부, 알타이 산맥과 톈산 산맥 사이에 끼여 있으며 동부는 해발 1,000m, 서부는 해발 500m이다. 이 문서에는 다음커뮤니케이션(현 카카오)에서 GFDL 또는 CC-SA 라이선스로 배포한 글로벌 세계대백과사전의 내용을 기초로 작성된 글이 포함되어 있습니다. (ko) ジュンガル盆地、ジュンガリア（モンゴル語: Зүүнгар / Züüngar, ウイグル語: جۇڭغار_ئويمانلىقى, 中国語: 准噶尔盆地）は中華人民共和国新疆ウイグル自治区の北西部にある盆地を中心とした土地である。面積はおおよそ77万7000平方キロメートル。 (ja) Kotlina Dżungarska (chiń. upr. 准噶尔盆地; chiń. trad. 準噶爾盆地; pinyin Zhǔngá’ěr Péndì) – tektoniczna kotlina w północno-zachodnich Chinach, między Tienszan i Ałtajem, o powierzchni ok. 380 tys. km² i wysokości 500-1000 m. W centralnej części kotliny znajduje się piaszczysta pustynia Gurbantünggüt, natomiast na obrzeżach suche stepy. Na całym obszarze występuje duża liczba słonych jezior. W kotlinie eksploatowane są m.in.: ropa naftowa, węgiel kamienny oraz złoto. (pl) 准噶尔盆地（蒙古语：ᠵᠡᠭᠦᠨ ᠭᠠᠷ，鲍培转写：jegün ɣar，西里尔字母：Зүүнгар ，意为“左手”）位于新疆的北部，是中国第二大的内陆盆地，在天山、阿尔泰山及西部的一些山脉之间。 (zh) |
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| dbp:s | 准噶尔盆地 (en) |
| dbp:t | 準噶爾盆地 (en) |
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| dct:subject | dbc:Sedimentary_basins_of_Asia dbc:Geology_of_Xinjiang |
| rdfs:comment | 중가르 분지(중국어 간체자: 准噶尔, 정체자: 準噶爾, 병음: Zhǔngáěr)는 중화인민공화국 신장 위구르 자치구의 북부, 알타이 산맥과 톈산 산맥 사이에 끼여 있으며 동부는 해발 1,000m, 서부는 해발 500m이다. 이 문서에는 다음커뮤니케이션(현 카카오)에서 GFDL 또는 CC-SA 라이선스로 배포한 글로벌 세계대백과사전의 내용을 기초로 작성된 글이 포함되어 있습니다. (ko) ジュンガル盆地、ジュンガリア（モンゴル語: Зүүнгар / Züüngar, ウイグル語: جۇڭغار_ئويمانلىقى, 中国語: 准噶尔盆地）は中華人民共和国新疆ウイグル自治区の北西部にある盆地を中心とした土地である。面積はおおよそ77万7000平方キロメートル。 (ja) Kotlina Dżungarska (chiń. upr. 准噶尔盆地; chiń. trad. 準噶爾盆地; pinyin Zhǔngá’ěr Péndì) – tektoniczna kotlina w północno-zachodnich Chinach, między Tienszan i Ałtajem, o powierzchni ok. 380 tys. km² i wysokości 500-1000 m. W centralnej części kotliny znajduje się piaszczysta pustynia Gurbantünggüt, natomiast na obrzeżach suche stepy. Na całym obszarze występuje duża liczba słonych jezior. W kotlinie eksploatowane są m.in.: ropa naftowa, węgiel kamienny oraz złoto. (pl) 准噶尔盆地（蒙古语：ᠵᠡᠭᠦᠨ ᠭᠠᠷ，鲍培转写：jegün ɣar，西里尔字母：Зүүнгар ，意为“左手”）位于新疆的北部，是中国第二大的内陆盆地，在天山、阿尔泰山及西部的一些山脉之间。 (zh) Džungarská pánev (ujgursky جۇڭغار ئويمانلىقى, Jungghar oymanliqi, čínsky 准噶尔盆地, Junggar Pendi, pinyin Zhǔngáěr Péndì, český přepis Čun-ka-er pchen-ti) je oblast na severozápadě Ujgurska a Čínské lidové republiky, mezi pohořími Altaj na severu, Ťan-šan na jihu a Tarbagataj (který se někdy považuje za součást Ťan-šanu) na západě. Nadmořská výška kolísá, místy překračuje i 1000 m, ale hladina jezera Ebinur v jihozápadním cípu pánve leží pouze 190 m n. m. Podstatnou část pánve vyplňuje druhá největší čínská poušť . Většina pánve je bez odtoku, pouze její severní částí protéká řeka Irtyš (Ertis Che). (cs) The Junggar Basin (simplified Chinese: 准噶尔盆地; traditional Chinese: 準噶爾盆地) is one of the largest sedimentary basins in Northwest China. It is located in Xinjiang, and enclosed by the Tarbagatai Mountains of Kazakhstan in the northwest, the Altai Mountains of Mongolia in the northeast, and the Heavenly Mountains (Tian Shan) in the south. The geology of Junggar Basin mainly consists of sedimentary rocks underlain by igneous and metamorphic basement rocks. The basement of the basin was largely formed during the development of the Pangea supercontinent during complex tectonic events from Precambrian to late Paleozoic time. The basin developed as a series of foreland basins – in other words, basins developing immediately in front of growing mountain ranges – from Permian time to the Quaternary p (en) |
| rdfs:label | Džungarská pánev (cs) Junggar Basin (en) ジュンガル盆地 (ja) 중가르 분지 (ko) Kotlina Dżungarska (pl) 准噶尔盆地 (zh) |
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