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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Bibliographic Details
Main Authors: López, Iván, Martín, Lucía, D’Incecco, Piero, Lang, Nicholas P., Di Achille, Gaetano
Other Authors: Agenzia Spaziale Italiana
Format: artículo biblioteca
Language:English
Published: Taylor & Francis 2023-09-06
Subjects:Venus, planetary geology, Imdr regio, large topographic rises,
Online Access:http://hdl.handle.net/10261/336636
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spelling 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
institution IPNA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-ipna-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IPNA España
language English
topic Venus
planetary geology
Imdr regio
large topographic rises
Venus
planetary geology
Imdr regio
large topographic rises
spellingShingle 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
description 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
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