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首页> 外文期刊>Bulletin of Canadian Petroleum Geology >Sedimentary basins and basement highs beneath the polar shelf north of Axel Heiberg and Meighen Islands
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Sedimentary basins and basement highs beneath the polar shelf north of Axel Heiberg and Meighen Islands

机译:阿克塞尔·海贝格岛和梅根群岛以北极地架下的沉积盆地和基底高点

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A seismic refraction program was carried out on the northeastern polar continental shelf north of Axel Heiberg and Meighen islands, Five distinct velocity units were identified throughout the area, The deepest unit, velocity unit 1, has velocities of 8.2 km/sec and represents the ultramafic, uppermost mantle, The top of this unit is the MOHO and it is about 25 km deep on the inner shelf and rises to 20 km on the outer shelf. The next velocity unit (2) has velocities of 6.6 to 6.8 km/sec and correlates well with the crystalline lower crust. Velocity unit 3 is characterized by velocities of 5.9 to 6.2 km/sec and is interpreted to consist primarily of highly indurated elastic and carbonate strata, volcanics and intrusives of the highly deformed, late Proterozoic to early Paleozoic Franklinian Basin. Along the shelf edge this unit may also encompass Lower Cretaceous volcanic flows and Jurassic-Cretaceous strata which are extensively intruded by sills and dykes. The top of this unit is considered to be "basement". Velocity unit 4 has velocities between 4.3 and 5.3 km/sec and is interpreted to consist mainly of mid Jurassic to Paleogene deltaic to basinal elastic strata, This unit is up to 10 km thick and occurs throughout the study area except over an offshore extension of the Princess Margaret Arch on the inner shelf and the crest of a prominent shelf edge high. The strata encompassed by this unit are likely deformed by folds and faults generated during the early Tertiary Eurekan Orogeny. Velocity unit 5 has velocities of 1.9 to 3.4 km/sec and probably comprises the undeformed Neogene succession, This unit is a few kilometres thick over much of the shelf and may include buried Upper Cretaceous-Paleogene strata on the inner shelf. The potential of the deformed Cretaceous-Paleogene succession to contain hydrocarbons is high but the presence of the Arctic ice pack over the area hampers traditional exploration. References: 41
机译:在阿克塞尔·海伯格岛和梅根岛以北的东北极地大陆架上进行了地震折射计划,在整个地区确定了五个不同的速度单位,最深的单位,速度单位1,速度为8.2公里/秒,代表超基性,最上地幔,该单元的顶部是MOHO,它在内架上深约25公里,在外架上上升到20公里。下一个速度单位(2)的速度为6.6至6.8公里/秒,与结晶下地壳密切相关。速度单元 3 的特点是速度为 5.9 至 6.2 公里/秒,被解释为主要由高度硬化的弹性和碳酸盐岩地层、火山岩和高度变形的晚元古代至早古生代富兰克林盆地的侵入岩组成。沿着陆架边缘,该单元还可能包括下白垩纪火山流和侏罗纪-白垩纪地层,这些地层被门槛和岩脉广泛侵入。该单元的顶部被认为是“地下室”。速度单元 4 的速度在 4.3 至 5.3 公里/秒之间,被解释为主要由侏罗纪中期至古近纪三角洲到盆地弹性地层组成,该单元厚达 10 公里,分布在整个研究区域,除了内架上玛格丽特公主拱门的近海延伸部分和突出的大陆架边缘高的顶部。该单元所包含的地层可能因第三纪尤里坎造山运动早期产生的褶皱和断层而变形。速度单元 5 的速度为 1.9 至 3.4 公里/秒,可能包括未变形的新近纪演替,该单元在大部分大陆架上有几公里厚,可能包括内架上埋藏的上白垩纪-古近纪地层。变形的白垩纪-古近纪演替含有碳氢化合物的潜力很高,但该地区北极冰层的存在阻碍了传统的勘探。[参考文献: 41]

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