Geological history of Samodiva Mons shield volcano, and surrounding area, Quadrangle V-29, Venus

IF 2.4 3区地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of Volcanology and Geothermal Research Pub Date : 2025-02-18 DOI:10.1016/j.jvolgeores.2025.108296

D.G. Malyshev , R.E. Ernst , H. El Bilali , M.A. Ivanov , C.H.G. Braga , V.E. Rozhin , A.S. Shimolina

{"title":"Geological history of Samodiva Mons shield volcano, and surrounding area, Quadrangle V-29, Venus","authors":"D.G. Malyshev , R.E. Ernst , H. El Bilali , M.A. Ivanov , C.H.G. Braga , V.E. Rozhin , A.S. Shimolina","doi":"10.1016/j.jvolgeores.2025.108296","DOIUrl":null,"url":null,"abstract":"<div><div>Samodiva Mons is a large shield volcano (∼240 km in diameter, centered at 13.6° N, 291.0° E) located 1500 km ESE from Beta Regio. Detailed mapping (1:500,000 scale) using radar image and altimetry data from the Magellan mission was used to investigate the geological history of the volcano and its surrounding area. The study area is located in Quadrangle V-29, which extends from 11° to 16° N, 289° to 294° E and covers approximately 291,000 km<sup>2</sup> of which ∼80,000 km<sup>2</sup> is occupied by Samodiva Mons volcanic materials. Seven geological units were defined, mapped, and characterized: Samodiva Mons lava flows, small shield volcanoes, coronae material, plains material, tesserae, densely lineated plains, and impact craters. Also, we distinguished two structural units: graben-fissure systems (interpreted as dike swarms) and wrinkle ridges. Three geological stages of evolution of the study region are recognized, with Stages 1–2 being pre-Samodiva Mons and Stage 3 that is associated with Samodiva Mons activity. This stage largely postdates the emplacement of regional plains and was culminated by the formation of the Samodiva Mons volcanic construct.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"461 ","pages":"Article 108296"},"PeriodicalIF":2.4000,"publicationDate":"2025-02-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Volcanology and Geothermal Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0377027325000320","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}

引用次数: 0

Abstract

Samodiva Mons is a large shield volcano (∼240 km in diameter, centered at 13.6° N, 291.0° E) located 1500 km ESE from Beta Regio. Detailed mapping (1:500,000 scale) using radar image and altimetry data from the Magellan mission was used to investigate the geological history of the volcano and its surrounding area. The study area is located in Quadrangle V-29, which extends from 11° to 16° N, 289° to 294° E and covers approximately 291,000 km² of which ∼80,000 km² is occupied by Samodiva Mons volcanic materials. Seven geological units were defined, mapped, and characterized: Samodiva Mons lava flows, small shield volcanoes, coronae material, plains material, tesserae, densely lineated plains, and impact craters. Also, we distinguished two structural units: graben-fissure systems (interpreted as dike swarms) and wrinkle ridges. Three geological stages of evolution of the study region are recognized, with Stages 1–2 being pre-Samodiva Mons and Stage 3 that is associated with Samodiva Mons activity. This stage largely postdates the emplacement of regional plains and was culminated by the formation of the Samodiva Mons volcanic construct.

查看原文

微信好友朋友圈 QQ好友复制链接

本刊更多论文

求助全文

约1分钟内获得全文去求助

来源期刊

Journal of Volcanology and Geothermal Research 地学-地球科学综合

CiteScore

5.90

自引率

13.80%

发文量

183

审稿时长

19.7 weeks

期刊介绍： An international research journal with focus on volcanic and geothermal processes and their impact on the environment and society. Submission of papers covering the following aspects of volcanology and geothermal research are encouraged: (1) Geological aspects of volcanic systems: volcano stratigraphy, structure and tectonic influence; eruptive history; evolution of volcanic landforms; eruption style and progress; dispersal patterns of lava and ash; analysis of real-time eruption observations. (2) Geochemical and petrological aspects of volcanic rocks: magma genesis and evolution; crystallization; volatile compositions, solubility, and degassing; volcanic petrography and textural analysis. (3) Hydrology, geochemistry and measurement of volcanic and hydrothermal fluids: volcanic gas emissions; fumaroles and springs; crater lakes; hydrothermal mineralization. (4) Geophysical aspects of volcanic systems: physical properties of volcanic rocks and magmas; heat flow studies; volcano seismology, geodesy and remote sensing. (5) Computational modeling and experimental simulation of magmatic and hydrothermal processes: eruption dynamics; magma transport and storage; plume dynamics and ash dispersal; lava flow dynamics; hydrothermal fluid flow; thermodynamics of aqueous fluids and melts. (6) Volcano hazard and risk research: hazard zonation methodology, development of forecasting tools; assessment techniques for vulnerability and impact.