Geology of the Imdr Regio area of Venus
We present a 1:5,000,000 geological map of the Imdr Regio area of Venus. Geological mapping was conducted using synthetic aperture radar (SAR) images, altimetry and stereo-derived topography data from NASA's Magellan mission. The map covers an area of approximately 7.9 × 106 km2 and exhibits a variety of tectonic structures and units of volcanic origin related to the evolution of Imdr Regio and surrounding plains. We have differentiated primary structures related to the emplacement of the different units from tectonic structures that deform them. These structures are also organized between those that are regional in extent and those that are related to the evolution of local large tectono-volcanic structures. The units in the map area represent different geologic processes (e.g. volcanism) that took place during the evolution of the large topographic rise. Geologic mapping illustrates a complex evolution with different styles of deformation and volcanism in this part of the planet.
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Format: | artículo biblioteca |
Language: | English |
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Taylor & Francis
2023-09-06
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Subjects: | Venus, planetary geology, Imdr regio, large topographic rises, |
Online Access: | http://hdl.handle.net/10261/336636 |
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dig-ipna-es-10261-3366362023-10-05T12:52:51Z Geology of the Imdr Regio area of Venus López, Iván Martín, Lucía D’Incecco, Piero Lang, Nicholas P. Di Achille, Gaetano Agenzia Spaziale Italiana Venus planetary geology Imdr regio large topographic rises We present a 1:5,000,000 geological map of the Imdr Regio area of Venus. Geological mapping was conducted using synthetic aperture radar (SAR) images, altimetry and stereo-derived topography data from NASA's Magellan mission. The map covers an area of approximately 7.9 × 106 km2 and exhibits a variety of tectonic structures and units of volcanic origin related to the evolution of Imdr Regio and surrounding plains. We have differentiated primary structures related to the emplacement of the different units from tectonic structures that deform them. These structures are also organized between those that are regional in extent and those that are related to the evolution of local large tectono-volcanic structures. The units in the map area represent different geologic processes (e.g. volcanism) that took place during the evolution of the large topographic rise. Geologic mapping illustrates a complex evolution with different styles of deformation and volcanism in this part of the planet. This research was partially supported by Italian Space Agency (ASI/2020-15-HH.0 and ASI/2022-15-HH.0 agreements). Peer reviewed 2023-10-05T12:52:51Z 2023-10-05T12:52:51Z 2023-09-06 artículo Journal of Maps, 19(1), 2253832 : 1-13 (2023) http://hdl.handle.net/10261/336636 10.1080/17445647.2023.2253832 1744-5647 en Publisher's version https://doi.org/10.1080/17445647.2023.2253832 Sí open Taylor & Francis |
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Venus planetary geology Imdr regio large topographic rises Venus planetary geology Imdr regio large topographic rises |
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Venus planetary geology Imdr regio large topographic rises Venus planetary geology Imdr regio large topographic rises López, Iván Martín, Lucía D’Incecco, Piero Lang, Nicholas P. Di Achille, Gaetano Geology of the Imdr Regio area of Venus |
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We present a 1:5,000,000 geological map of the Imdr Regio area of Venus. Geological mapping was conducted using synthetic aperture radar (SAR) images, altimetry and stereo-derived topography data from NASA's Magellan mission. The map covers an area of approximately 7.9 × 106 km2 and exhibits a variety of tectonic structures and units of volcanic origin related to the evolution of Imdr Regio and surrounding plains. We have differentiated primary structures related to the emplacement of the different units from tectonic structures that deform them. These structures are also organized between those that are regional in extent and those that are related to the evolution of local large tectono-volcanic structures. The units in the map area represent different geologic processes (e.g. volcanism) that took place during the evolution of the large topographic rise. Geologic mapping illustrates a complex evolution with different styles of deformation and volcanism in this part of the planet. |
author2 |
Agenzia Spaziale Italiana |
author_facet |
Agenzia Spaziale Italiana López, Iván Martín, Lucía D’Incecco, Piero Lang, Nicholas P. Di Achille, Gaetano |
format |
artículo |
topic_facet |
Venus planetary geology Imdr regio large topographic rises |
author |
López, Iván Martín, Lucía D’Incecco, Piero Lang, Nicholas P. Di Achille, Gaetano |
author_sort |
López, Iván |
title |
Geology of the Imdr Regio area of Venus |
title_short |
Geology of the Imdr Regio area of Venus |
title_full |
Geology of the Imdr Regio area of Venus |
title_fullStr |
Geology of the Imdr Regio area of Venus |
title_full_unstemmed |
Geology of the Imdr Regio area of Venus |
title_sort |
geology of the imdr regio area of venus |
publisher |
Taylor & Francis |
publishDate |
2023-09-06 |
url |
http://hdl.handle.net/10261/336636 |
work_keys_str_mv |
AT lopezivan geologyoftheimdrregioareaofvenus AT martinlucia geologyoftheimdrregioareaofvenus AT dinceccopiero geologyoftheimdrregioareaofvenus AT langnicholasp geologyoftheimdrregioareaofvenus AT diachillegaetano geologyoftheimdrregioareaofvenus |
_version_ |
1781881406970920960 |