东西伯利亚盆地和北楚科奇盆地白垩-新生代古地理,东北极陆架

A. Medvedev, V. Ershova, A. Khudoley, O. Makhova, I. Vasilieva, V. S. Vinnikovskiy, A. Popova, N. Malyshev, V. Verzhbitskiy, V. V. Obmetko, A. A. Borodulin, B. I. Ikhsanov
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引用次数: 0

摘要

东西伯利亚海陆架和北楚科奇海陆架是早白垩世-晚白垩世和新生代三角洲沉积强烈的地区。大型三角洲系统向前推进了数百公里,形成了大陆梯田。厚沉积充填与两个碎屑脉冲有关:aptian -晚白垩世和新生代。许多古地理图反映了主要的沉积时代。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Cretaceous-cenozoic Paleogeography of East-siberian and North Chuckchi Basins, Shelf of East Arctic
East-Siberian and North Chuckchi seas shelfs was the area of intensive deltaic sedimentation during Aptian-Late Cretaceous and Cenozoic times. Large deltaic systems prograded at distance of hundreds kilometers building up continental terraces. Thick sedimentary infill related to two clastic pulses: Aptian-Late Cretaceous and Cenozoic. A number of a paleogeographic maps reflect the major sedimentary epochs.
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