EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE

The Gamburtsev Subglacial Mountains (GSM), located in the central East Antarctica, were discovered by the Soviet team of the 3rd Complex Antarctic Expedition in 1958-1959. The GSM has highly dissected Alpine topography reaching maximum elevations of 3000 m. The mechanism driving uplift of the young-...

Full description

Bibliographic Details
Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Author: Pavel G. Talalay
Format: Article in Journal/Newspaper
Language:English
Published: Lomonosov Moscow State University 2014
Subjects:
geo
Online Access:https://doi.org/10.24057/2071-9388-2014-7-1-5-15
https://doaj.org/article/f94e30e9c45448e2938461164fc783d2
id fttriple:oai:gotriple.eu:oai:doaj.org/article:f94e30e9c45448e2938461164fc783d2
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:f94e30e9c45448e2938461164fc783d2 2023-05-15T13:41:27+02:00 EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE Pavel G. Talalay 2014-03-01 https://doi.org/10.24057/2071-9388-2014-7-1-5-15 https://doaj.org/article/f94e30e9c45448e2938461164fc783d2 en eng Lomonosov Moscow State University 2071-9388 2542-1565 doi:10.24057/2071-9388-2014-7-1-5-15 https://doaj.org/article/f94e30e9c45448e2938461164fc783d2 undefined Geography, Environment, Sustainability, Vol 7, Iss 1, Pp 5-15 (2014) subglacial environment antarctic tectonics bedrock drilling geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2014 fttriple https://doi.org/10.24057/2071-9388-2014-7-1-5-15 2023-01-22T19:23:26Z The Gamburtsev Subglacial Mountains (GSM), located in the central East Antarctica, were discovered by the Soviet team of the 3rd Complex Antarctic Expedition in 1958-1959. The GSM has highly dissected Alpine topography reaching maximum elevations of 3000 m. The mechanism driving uplift of the young-shaped GSM in the middle of the old East Antarctic Shield is unknown. With only limited constraints available on the topography, geology, and lithospheric structure, the origin of the GSM has been a matter of considerable speculation. The latest interpretation suggested that the GSM were formed during Permian and Cretaceous (roughly 250-100 Ma ago) due to the combination of rift-flank uplift, root buoyancy and the isostatic response. Later on the Antarctic Ice Sheet covered the range and protected it from erosion. However, this theory cannot explain lack of erosion process during many millions years in between uplifting and beginning of glaciation. The next step of the GSM exploration focuses on the direct observation of ice sheet bed by drilling. In order to penetrate into subglacial bedrock in the GSM region the development activity already has been started in China. It is proposed to use cable-suspended drilling technology and movable drilling shelter that can be transported to the chosen site with crawler-tractor. The first field tests of the drilling equipment are planned to carry out near Antarctic coast in season 2015-2016, and drilling to the bedrock would be finished during next two seasons. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Unknown Antarctic East Antarctica Gamburtsev Subglacial Mountains ENVELOPE(76.000,76.000,-80.500,-80.500) The Antarctic GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 7 1 5 15
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic subglacial environment
antarctic tectonics
bedrock drilling
geo
spellingShingle subglacial environment
antarctic tectonics
bedrock drilling
geo
Pavel G. Talalay
EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE
topic_facet subglacial environment
antarctic tectonics
bedrock drilling
geo
description The Gamburtsev Subglacial Mountains (GSM), located in the central East Antarctica, were discovered by the Soviet team of the 3rd Complex Antarctic Expedition in 1958-1959. The GSM has highly dissected Alpine topography reaching maximum elevations of 3000 m. The mechanism driving uplift of the young-shaped GSM in the middle of the old East Antarctic Shield is unknown. With only limited constraints available on the topography, geology, and lithospheric structure, the origin of the GSM has been a matter of considerable speculation. The latest interpretation suggested that the GSM were formed during Permian and Cretaceous (roughly 250-100 Ma ago) due to the combination of rift-flank uplift, root buoyancy and the isostatic response. Later on the Antarctic Ice Sheet covered the range and protected it from erosion. However, this theory cannot explain lack of erosion process during many millions years in between uplifting and beginning of glaciation. The next step of the GSM exploration focuses on the direct observation of ice sheet bed by drilling. In order to penetrate into subglacial bedrock in the GSM region the development activity already has been started in China. It is proposed to use cable-suspended drilling technology and movable drilling shelter that can be transported to the chosen site with crawler-tractor. The first field tests of the drilling equipment are planned to carry out near Antarctic coast in season 2015-2016, and drilling to the bedrock would be finished during next two seasons.
format Article in Journal/Newspaper
author Pavel G. Talalay
author_facet Pavel G. Talalay
author_sort Pavel G. Talalay
title EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE
title_short EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE
title_full EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE
title_fullStr EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE
title_full_unstemmed EXPLORATION OF GAMBURTSEV SUBGLACIAL MOUNTAINS (EAST ANTARCTICA): BACKGROUND AND PLANS FOR THE NEAR FUTURE
title_sort exploration of gamburtsev subglacial mountains (east antarctica): background and plans for the near future
publisher Lomonosov Moscow State University
publishDate 2014
url https://doi.org/10.24057/2071-9388-2014-7-1-5-15
https://doaj.org/article/f94e30e9c45448e2938461164fc783d2
long_lat ENVELOPE(76.000,76.000,-80.500,-80.500)
geographic Antarctic
East Antarctica
Gamburtsev Subglacial Mountains
The Antarctic
geographic_facet Antarctic
East Antarctica
Gamburtsev Subglacial Mountains
The Antarctic
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
op_source Geography, Environment, Sustainability, Vol 7, Iss 1, Pp 5-15 (2014)
op_relation 2071-9388
2542-1565
doi:10.24057/2071-9388-2014-7-1-5-15
https://doaj.org/article/f94e30e9c45448e2938461164fc783d2
op_rights undefined
op_doi https://doi.org/10.24057/2071-9388-2014-7-1-5-15
container_title GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
container_volume 7
container_issue 1
container_start_page 5
op_container_end_page 15
_version_ 1766150967308320768