Tectonics of the Drake Passage-Scotia Sea Zone in the Southern Ocean

被引：4

作者：

Udintsev, G. B. ^{[1
]}

Kurentsova, N. A. ^{[1
]}

Beresnev, A. F. ^{[1
]}

Kol'tsova, A. V. ^{[1
]}

Domoratskaya, L. G. ^{[1
]}

Schenke, G. V. ^{[2
]}

Bakhmutov, V. G. ^{[3
]}

Solov'ev, V. D. ^{[3
]}

机构：

[1] Russian Acad Sci, Vernadsky Inst Geochem & Analyt Chem, Moscow, Russia

[2] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany

[3] Natl Acad Sci Ukraine, Inst Geophys, Kiev, Ukraine

来源：

DOKLADY EARTH SCIENCES | 2012年 / 445卷 / 02期

关键词：

DOKLADY Earth Science; Antarctic Peninsula; Drake Passage; Scotia Ridge; Deep Water Drilling;

D O I：

10.1134/S1028334X12080260

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The relief and geophysical characteristics of the sea floor in the Drake Passage-Scotia Sea zone have been studied quite well in general. The oceanic floor within this zone is usually considered as a collage of small fragments of the continental bridge and of young oceanic plates formed by spreading under the large-scale motions of large lithospheric plates. The authors suppose an alternative version of the genesis of the Drake Passage-Scotia Sea lithospheric zone as an area of large fragments of the continental bridge subjected to basification under the conditions of temperate extension and local rifting.

引用

页码：1029 / 1035

页数：7

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