Tectonic feature of the Western Barents Sea and its evolution
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摘要:
巴伦支海陆架宽广，油气资源丰富，其南部是北极地区调查程度相对较高的海域。该区沉积基底主体形成于加里东期，包括西部的加里东造山带、中部的斯瓦尔巴—喀拉微板块、东南的蒂曼造山带，东缘为新地岛褶皱带。西巴伦支海构造以台地与小型盆地相间格局为特征，发育3组裂谷盆地群：泥盆纪末—早石炭世、晚侏罗世—早白垩世和晚白垩世—新近纪裂谷盆地群。加里东之后，巴伦支海地壳处于拉伸状态，形成一系列NE向裂谷盆地。晚石炭世开始，裂谷作用停止，以区域沉降为主。二叠纪—三叠纪巴伦支海东缘的新地岛褶皱带碰撞隆升，完全改变了巴伦支海物源格局，由早期的西部物源为主变为西南为主。中侏罗世晚期—早白垩世，西南巴伦支海老的线性构造复活，形成新裂谷盆地。晚白垩世—新生代，巴伦支海西缘边缘持续沉降，形成裂谷。除西缘外，西巴伦支海新生代以区域的隆升剥蚀为主，对生烃和油气藏储产生重大影响。
Abstract:There are rich petroleum resources in the Barents Sea which has a wide shelf. The southern part of the sea is relatively well explored. The basement of the Barents Sea shelf is formed in the time of Caledonian, which includes the Caledonian orogenic belt in west, the Svalbard-Kara microplate in centre, the Timan orogenic belt in Southeast and the Novozemelskiy fold belt in east. The western Barents Sea is characterized by a number of small basins and platforms. There are three groups of rift basins, developed in the end of Devonian-early Carboniferous, the Late Jurassic-early Cretaceous and the late Cretaceous-Cenozoic respectively. After the Caledonian, the crust of the Barents Sea was under stretching, which lead to a series of NE rift basins. From late Carboniferous, however, the rifting was ended, and followed by regional subsidence. During Permian-Triassic period, the Novozemelskiy fold belt was uplifting due to the colliding in the east edge of the Barents Sea. As the result, the provenance pattern of the Barents Sea was completely changed from west to southeast. During the end of Middle Jurassic to the early Cretaceous, the old linear structures were reactivated in the southwestern Barents Sea and new rift basins formed. The west margin of the Barents Sea was subsiding continually to be rift troughs. In addition to the west margin, the uplifting and erosion prevailed in the rest of the western Barents Sea, which brought significant influence to hydrocarbon generation and accumulation.
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Key words:
- stratigraphy /
- sedimentary basins /
- tectonic evolution /
- the Barents Sea
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