New Data on the Geological Structure of the Junction of the Cape Verde Rise, Cape Verde Abyssal Basin, and Bathymetrists Seamounts (Central Atlantic Ocean)

S. G. Skolotnev; N. N. Turko; S. Yu. Sokolov; A. A. Peyve; N. V. Tsukanov; S. Yu. Kolodyazhnyi; N. P. Chamov; Yu. E. Baramykov; A. S. Ponomarev; V. N. Efimov; A. E. Eskin; V. V. Petrova; L. A. Golovina; V. Yu. Lavrushin; E. A. Letyagina; E. P. Shevchenko

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New Data on the Geological Structure of the Junction of the Cape Verde Rise, Cape Verde Abyssal Basin, and Bathymetrists Seamounts (Central Atlantic Ocean)

机译：佛得角崛起，佛得角深渊盆地和深海浮标海山交界处的地质结构的新数据（中大西洋）

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According to the plate tectonics concept, Atlantictype oceanic margins belong to tectonically passive margins. However, many observations indicate that some segments of these margins are characterized by intense tectonic and magmatic activity [1]. Cruise 23 of the R/V Akademik Nikolai Strakhov was accomplished in one such region at the junction of the continental slope and Atlantic Ocean structures south of the Cape Verde Islands (Fig. 1). The scientific supervisors of the cruise were Academician Yu.M. Pushcharovsky and Yu.G. Leonov. In the cruise, the bottom topography and acoustic profiling were studied with a RESON (SeaBat 8150) multibeam echo sounder, continuous seismic profiling (CSP) was carried out, magnetic and gravitation fields were measured, and dredging and sampling of bottom sediments were also conducted.

机译：根据板块构造概念，大西洋型海洋边缘属于构造被动边缘。然而，许多观察表明，这些边缘的某些部分具有强烈的构造和岩浆活动特征[1]。 R / V Akademik Nikolai Strakhov的23号巡航是在佛得角群岛以南的大陆斜坡和大西洋结构交界处的一个这样的区域完成的（图1）。邮轮的科学主管是俞宇明院士。普什恰洛夫斯基和尤格列昂诺夫。在航行中，使用RESON（SeaBat 8150）多波束回声测深仪研究了底部地形和声波轮廓，进行了连续地震波轮廓（CSP），测量了磁场和重力场，还对底部沉积物进行了疏ging和采样。

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《Doklady Earth Sciences》 |2007年第7期|p.1037-1041|共5页
作者
S. G. Skolotnev; N. N. Turko; S. Yu. Sokolov; A. A. Peyve; N. V. Tsukanov; S. Yu. Kolodyazhnyi; N. P. Chamov; Yu. E. Baramykov; A. S. Ponomarev; V. N. Efimov; A. E. Eskin; V. V. Petrova; L. A. Golovina; V. Yu. Lavrushin; E. A. Letyagina; E. P. Shevchenko;
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Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia;

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正文语种 eng
中图分类天文学、地球科学;
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1. New Data on the Geological Structure of the Junction between the Cape Verde Seamount and the Cape Verde Basin, Central Atlantic [J] . S. G. Skolotnev, A. A. Peive, N. N. Turko, Doklady Earth Sciences . 2006,第1a2期

机译：大西洋中部佛得角海山与佛得角盆地交界处的地质结构新数据
2. New Data on the Structure of Sedimentary Cover at the Cape Verde Seamount and the Cape Verde Basin (Central Atlantic) Based on Continuous Seismic Profiling Data [J] . V. N. Efimov, S. G. Skolotnev Doklady Earth Sciences . 2006,第3期

机译：基于连续地震剖面数据的佛得角海山和佛得角盆地（中大西洋）沉积盖结构的新数据
3. Neotectonic morphotructures in the junction zone of the Cape Verde Rise and Cape Verde Abyssal Plain, Central Atlantic [J] . S G Skolotnev S Yu Kolodyazhny N V Tsukanov N P Chamov S Yu Sokolov Geotectonics . 2009,第1期

机译：大西洋中部佛得角上升与佛得角深渊平原交界处的新构造形态构造
4. OCEANOGRAPHIC CHARACTERISATION OF THE CAPE VERDE REGION USINGMULTISENSOR DATA [C] . M. J. Fernandes, C. Lázaro, A. M. P. Santos, 2004 Envisat amp; ERS symposium . 2004

机译：利用多传感器数据对佛得角地区进行海洋学表征
5. Tropical Atlantic climate variability recorded in corals from the Cape Verde Islands and the eastern Caribbean. [D] . Moses, Christopher Stanton. 2005

机译：佛得角群岛和东加勒比海地区的珊瑚中记录到热带大西洋气候变化。
6. Population size breeding biology and on-land threats of Cape Verde petrel (Pterodroma feae) in Fogo Island Cape Verde [O] . Teresa Militão, Herculano Andrade Dinis, Laura Zango, -1

机译：佛得角福戈岛的佛得角海燕（Pterodroma feae）的种群数量繁殖生物学和陆上威胁
7. Concept of Biogenic Ferromanganese Crust Formation: Coccoliths as Bio-seeds in Crusts from Central Atlantic Ocean (Senghor Seamount/Cape Verde) [O] . Xiaohong Wang, Florian Peine, Alexander Schmidt, 2011

机译：生物原生铁锰料壳的概念形成：Coccoliths作为中央大西洋中央大西洋地壳中的生物种子（Senghor Seamount / Cape Verde）
8. Abyssal Benthonic Foraminifera and the Carbonate Saturation of Sea Water and a Benthonic Foraminiferal Carbonate Saturation History for the Cape Verde Basin for the Last 550,000 Years [R] . Bremer, M. L. 1983

机译：近500年来佛得角盆地深海底栖动物有孔虫和海水碳酸盐饱和度及底栖有孔虫碳酸盐饱和度历史

New Data on the Geological Structure of the Junction of the Cape Verde Rise, Cape Verde Abyssal Basin, and Bathymetrists Seamounts (Central Atlantic Ocean)

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