TASMANDRAKE Cruise, RV Hespérides

TASMANDRAKE Cruise (29HE20180111) carried out on the Research Vessel Hespérides in 2018 The general objective of the TASMANDRAKE project is the study of the onset and evolution of the Antarctic Circumpolar Current (ACC). Taking into account the allowed period and that the capabilities of the geophys...

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Main Authors: Escutia, Carlota, Bohoyo, Fernando, CSIC - Unidad de Tecnología Marina (UTM)
Format: Dataset
Language:unknown
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/10261/231982
https://doi.org/10.20351/29HE20180111
id ftcsic:oai:digital.csic.es:10261/231982
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/231982 2024-02-11T09:58:02+01:00 TASMANDRAKE Cruise, RV Hespérides Escutia, Carlota Bohoyo, Fernando CSIC - Unidad de Tecnología Marina (UTM) 2018 http://hdl.handle.net/10261/231982 https://doi.org/10.20351/29HE20180111 unknown https://doi.org/10.20351/29HE20180111 http://hdl.handle.net/10261/231982 doi:10.20351/29HE20180111 none dataset http://purl.org/coar/resource_type/c_ddb1 2018 ftcsic https://doi.org/10.20351/29HE20180111 2024-01-16T11:03:50Z TASMANDRAKE Cruise (29HE20180111) carried out on the Research Vessel Hespérides in 2018 The general objective of the TASMANDRAKE project is the study of the onset and evolution of the Antarctic Circumpolar Current (ACC). Taking into account the allowed period and that the capabilities of the geophysical equipment on board cannot image the deep structures and sediments, the cruise cannot fulfill the objectives of the TASMANDRAKE Project pertaining to the opening of gateways and onset of the ACC. We have therefore developed and alternative plan for the DRAKE2018 cruise that will allow us to collect mid-penetration to shallow data from the southern Drake-Scotia area (58ºS/62ºS and 60ºW/50ºW) and the South Orkney Shelf (60ºS/63ºS and 50ºW/40ºW). With this kind of capabilities we target those objectives of the TASMANDRAKE Project dealing with: 1) the evolution of the ACC during the Pleistocene and the Holocene; and 2) near-surface structure of continental blocks (i.e., the South Orkney micro-continent and the platform surrounding Elephant Island) and age of the older oceanic crust in Drake Passage. The proposed work is aimed to help land- ocean correlations between the stratigraphy of Seymour/Marambio Island and Ocean Drilling Project Site 696, in order to better understand the break-up and paleogeographic evolution of these continental blocks. The proposed marine surveys will consist in the execution of predefined transects along which geophysical data will be collected. In addition, we expect to collect sediment cores in specific sites, in order to groundtruth seismic facies with sediment information and provide age constrains of the most recent (Quaternary-Pliocene) units Dataset Antarc* Antarctic Drake Passage Elephant Island Digital.CSIC (Spanish National Research Council) Antarctic Drake Passage Elephant Island ENVELOPE(-55.184,-55.184,-61.085,-61.085) Marambio ENVELOPE(-56.750,-56.750,-64.283,-64.283) Seymour ENVELOPE(-56.767,-56.767,-64.283,-64.283) The Antarctic
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
description TASMANDRAKE Cruise (29HE20180111) carried out on the Research Vessel Hespérides in 2018 The general objective of the TASMANDRAKE project is the study of the onset and evolution of the Antarctic Circumpolar Current (ACC). Taking into account the allowed period and that the capabilities of the geophysical equipment on board cannot image the deep structures and sediments, the cruise cannot fulfill the objectives of the TASMANDRAKE Project pertaining to the opening of gateways and onset of the ACC. We have therefore developed and alternative plan for the DRAKE2018 cruise that will allow us to collect mid-penetration to shallow data from the southern Drake-Scotia area (58ºS/62ºS and 60ºW/50ºW) and the South Orkney Shelf (60ºS/63ºS and 50ºW/40ºW). With this kind of capabilities we target those objectives of the TASMANDRAKE Project dealing with: 1) the evolution of the ACC during the Pleistocene and the Holocene; and 2) near-surface structure of continental blocks (i.e., the South Orkney micro-continent and the platform surrounding Elephant Island) and age of the older oceanic crust in Drake Passage. The proposed work is aimed to help land- ocean correlations between the stratigraphy of Seymour/Marambio Island and Ocean Drilling Project Site 696, in order to better understand the break-up and paleogeographic evolution of these continental blocks. The proposed marine surveys will consist in the execution of predefined transects along which geophysical data will be collected. In addition, we expect to collect sediment cores in specific sites, in order to groundtruth seismic facies with sediment information and provide age constrains of the most recent (Quaternary-Pliocene) units
format Dataset
author Escutia, Carlota
Bohoyo, Fernando
CSIC - Unidad de Tecnología Marina (UTM)
spellingShingle Escutia, Carlota
Bohoyo, Fernando
CSIC - Unidad de Tecnología Marina (UTM)
TASMANDRAKE Cruise, RV Hespérides
author_facet Escutia, Carlota
Bohoyo, Fernando
CSIC - Unidad de Tecnología Marina (UTM)
author_sort Escutia, Carlota
title TASMANDRAKE Cruise, RV Hespérides
title_short TASMANDRAKE Cruise, RV Hespérides
title_full TASMANDRAKE Cruise, RV Hespérides
title_fullStr TASMANDRAKE Cruise, RV Hespérides
title_full_unstemmed TASMANDRAKE Cruise, RV Hespérides
title_sort tasmandrake cruise, rv hespérides
publishDate 2018
url http://hdl.handle.net/10261/231982
https://doi.org/10.20351/29HE20180111
long_lat ENVELOPE(-55.184,-55.184,-61.085,-61.085)
ENVELOPE(-56.750,-56.750,-64.283,-64.283)
ENVELOPE(-56.767,-56.767,-64.283,-64.283)
geographic Antarctic
Drake Passage
Elephant Island
Marambio
Seymour
The Antarctic
geographic_facet Antarctic
Drake Passage
Elephant Island
Marambio
Seymour
The Antarctic
genre Antarc*
Antarctic
Drake Passage
Elephant Island
genre_facet Antarc*
Antarctic
Drake Passage
Elephant Island
op_relation https://doi.org/10.20351/29HE20180111
http://hdl.handle.net/10261/231982
doi:10.20351/29HE20180111
op_rights none
op_doi https://doi.org/10.20351/29HE20180111
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