Stratigraphy of sediments from the Hakon Mosby Mud Volcano Area

被引：7

作者：

Shilov, VV ^{[1
]}

Druzhinina, NI ^{[1
]}

Vasilenko, LV ^{[1
]}

Krupskaya, VV ^{[1
]}

机构：

[1] Inst Geol & Mineral Resources Ocean, VNIIOkeangeol, St Petersburg, Russia

来源：

GEO-MARINE LETTERS | 1999年 / 19卷 / 1-2期

关键词：

D O I：

10.1007/s003670050092

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Studies of four gravity cores From the Hakon Mosby Mud Volcano area have shown the existence of three lithologic-stratigraphic units: I - brown clay (0-10 ka), II - gray clay (10-30 ka) and III - gray silt (30-61 ka). The units reflect different paleographic sedimentation and conditions, including the influence of mud volcanic activity. Two periods of mud volcanic activity can probably be discerned: 10-30 ka and Recent. The coexistence-of Pleistocene and Late Pliocene benthic foraminifera suggests that the source depth of the volcano is located below the Plioccene-Pleistocene boundary.

引用

页码：48 / 56

页数：9

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