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Schedule Overview  
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Mon, March 13 Tue, March 14 Wed, March 15 Thu, March 16 Fri, March 17

Poster Session: Venus: The Heat is On

Wednesday, March 15, 2023, 6:30 PM
iPosters/Gather.town

Budko K. S.* Ernst R. E. El Bilali H.
Geological History of Atai Mons Region, SE of Phoebe Regio, Venus [#1512]
Detailed mapping of graben-fissure lineaments is revealing the dyke swarm history of Atira Mons, and other magmatic centres, SE of Phoebe Regio, Venus.
Ankach M.* El Bilali. H. Ernst. R. E. Head. J. W. Youbi. N.
Sapas Mons, Atla Regio, Venus: Anatomy of a Very Large Shield Volcano [#1717]
Sapas Mons is a large, 600-km-diameter, 2.4-km-high (relative to surrounding plains) shield volcano in the Atla Regio area of Venus.
Tessier A. D.* Ernst R. E. El Bilali H.
Geological History of Heng-o Corona, Venus [#1131]
Detailed mapping of grabens and flows of Heng-o corona revealed a new circumferential ring that doubles its size. Flow/plains map. Comparison to HALIP.
Ben Marzoug M.* El Bilali H. Ernst R. E. Buchan K. L. Youbi N.
Quetzalpetlatl and Interior Boala Coronae, in Lada Terra Rise on Venus: Graben-Fissure Systems (Dyke Swarms) and Channelized Flows [#1153]
Dyke swarm history of the 850-km-diameter Quetzalpetlatl Corona and feeding of channelized flows from circumferential dykes of interior Boala Corona. .
Hannour N.* El Bilali H. Ernst R. E. Buchan K. L. Youbi N.
Dyke Swarms (Based On Overlying Graben Sets) Of Eastern Ovda Regio, Venus [#1155]
Detailed mapping of graben systems in eastern Ovda Regio and interpreting them as dyke swarms.
Shimolina A. S.* Ernst R. E. El Bilali H.
Lava Flows of Theia Mons Volcano, Beta Regio Plume Centre, Venus [#1159]
Theia Mons is one of the most important volcanic edifices on Venus centered at Beta Regio. It covers a large area by many lava flows of different sources.
Singh H.* Ernst R. E. El Bilali H. Srivastava R. K.
Dyke Swarm History of Nehalennia Corona Region, Central Eistla Regio, Venus [#1181]
Dyke swarms of Nehalennia corona region, Central Eistla Regio, Venus will help us to decipher the likely plume centres and geological history of this region.
Chaddha T.* Ernst R. E. El Bilali H. Srivastava R. K.
Dyke Swarm History of Belet-Ili Corona and Gaya Corona Region, Central Eistla Regio, Venus [#1182]
Dyke swarms of Belet-ili and Gaya Corona region, Central Eistla Regio would help to decipher magmatic centres and geological-tectonic history of this region.
Oukhro R.* El Bilali H. Ernst R. E. Head J. W. Youbi N.
Western Jokwa Linea Groove Belt, SE Stanton Quadrangle (V-38), Venus: Part Of Triple Junction Rift System [#1219]
Detailed mapping of western Jokwa Linea, Venus, reveals multiple magmatic centres, rifting with rift flank uplift and a triple junction rift system.
Ouaskioud K.* El Bilali H. Ernst R. E. Head J. W. Youbi N.
Geological Setting and History of Itoki Fluctus (Lava Flow System), Venus [#1292]
The 900-km-long Itoki fluctus formed at least three lava lakes that may have filled older corona.
Eloualda K.* EL Bilali H. Ernst R. E. Buchan K. L. Youbi N.
Dyke and Canali History Around Ituana Corona, LLorona Planitia, Venus [#1319]
Ituana Corona, associated dyke swarms, and the canali system around.
Hasanaine A.* El Bilali H. Ernst R. E. Youbi N.
Dyke Swarms of Ninmah Corona Area, Eastern Eistla Regio, Venus [#1338]
The dyke swarm record of the Ninmah corona area (Eastern Eistla Regio, Venus) is revealed through detailed mapping of graben-fissure systems.
Moutbir O. El Bilali H. Ernst R. E. Head J. W. Youbi N.
Characterization of a Caldera Cluster (21.5 N, 201.5 E), NE of Atla Regio Quadrangle (V-26), Venus [#1386]
Characterization of a Caldera cluster located in the north of Atla Regio.
Mediany M. A.* El Bilali H. Ernst R. E. Head J. W. Youbi N.
Graben Systems (Interpreted as Dyke Swarms) of Sith And Khabuchi Coronae Along Dali Chasma, Southwest of Atla Regio, Venus [#1397]
Dyke swarm history of Sith and Khabuchi Coronae, Dali Chasma, Venus.
Houane H.* EL Bilali H. Ernst R. E. Head J. W. Youbi N.
Dyke Swarm History of Corona Along the Hecate Chasmata in the Vicinity of Sobra Fluctus, Venus [#1437]
Many graben-fissure lineaments along the Hecate Chasmata in the vicinity of Sobra Fluctus with a huge fluctus that may be fed by coronae.
El Kamel Z.* El Bilali H. Ernst R. E. Youbi N.
Dyke Swarm History of SE Thaukhud Linea Region, Venus. [#1444]
Detailed mapping of graben-fissure lineaments to determine the dyke swarm history of Thaukhud linea region, Venus.
El-ouali L.* El Bilali H. Ernst R. E. Youbi N.
Dyke Swarm History of Lumimuut Corona Region, Venus [#1487]
Detailed mapping of graben-fissure lineaments for determining the dyke swarm history of the Lumimuut Corona region.
Hadimi I.* El Bilali H. Ernst R. E. Youbi N.
Nott Corona Region, Isabella Quadrangle (V-50), Venus: Detailed Mapping of Graben-Fissure Systems Identifies Critical Targets For Future Missions [#1704]
Detailed mapping of graben-fissure systems in the Nott Corona Region, Isabella Quadrangle (V-50), Venus to identify critical targets for the upcoming missions.
Ait Lahna A.* El Bilali H. Ernst R. E. Youbi N.
Normal Fault Kinematics Exposing the Venusian Crust in Dali Chasma, SW of Atla Regio: A Potential Target For Future Venus Missions [#1735]
Asymmetric rifting along Dali Chasma exposes a 4-km section through venusian crust; potential target for ground-penetrating radar in future mission.
Stark R.* Ernst R. E. El Bilali H. Head J. W.
Neago Fluctus, Venus: 3D-Visualization Provides New Insights into Source Regions and Emplacement History [#1816]
We use 3D Visualization Techniques through ArcGIS Local Scene function in order to take a closer and more intuitive look at a portion of Neago Fluctus.
Mghazli K.* El Bilali H. Ernst R. E. Buchan K. L. Youbi N.
Maram Corona, Venus: Affected by Faulting of Parga Chasmata [#1981]
The history of Maram Corona growth: The topographic changes and their link with host Parga Chasmata, southeast of Atla Regio, Venus.
Riaz M.* Ernst R. E. El Bilali H.
Dyke Swarms Of Bell Regio, Venus [#1510]
Detailed mapping of 10,800 graben-fissure lineaments were used to develop a preliminary dyke swarm history of Bell Regio.
Malyshev D. G.* Ernst R. E. El Bilali H. Ivanov M. A.
Lava Flows of Samodiva Mons Region, Southeast of Beta Regio, Venus [#1149]
Lava flows, graben swarms, regional plains and other geological units are described and unified in the history of Samodiva Mons formation.
Rozhin V. E.* Ernst R. E. El Bilali H.
Geological History of the Region of Polik-Mana Mons, Venus [#1626]
Polik-mana Mons volcano is located in the Asteria Regio lowlands along Latona Chasma, which is part of the 7000-km-long Hecate Chasmata rift zone.
Ounar J.* El Bilali H. Ernest R. E. Head J. W. Youbi N.
Extensional Lineaments of NW Wawalag Planitia, Stanton Quadrangle (V-38), Venus [#1697]
Extensional lineaments of NW Wawalag Planitia, Stanton Quadrangle (V-38), Venus.
Buczkowski D. L.* Fattaruso L. A. McGowan E. M. McGill G. E.
Structural Belt in the Lachesis Tessera Quadrangle (V-18), Venus: Implications for a Change in Crustal Proper-Ties? [#2302]
A progression from a high-standing fracture belt to low-lying coronae suggests a density interface and change in crustal thickness under the linear chain.
Dean R.* Ernst R. E. Bilali H. El. Buchan K. L.
Dyke Swarms and Triple Junction Rifting in Western Ovda Tessera, Venus [#1172]
Detailed mapping of graben sets (marking dyke swarms) in Western Ovda Regio, and recognition of triple junction rifting.
Guseva E. N.* Ivanov M. A.
Coronae-Sources of Younger Volcanism on Venus: Lack of Size-Eruptive Productivity Correlation [#1090]
Our analysis showed that the size of the parental diapir has little (if any) effect on the eruptive productivity of the coronae.
Adeli S.* Garland S. P. Gillespie J. Alemanno G. D’Amore M. et al.
VEM/VERITAS Analogs in the PSL Labratory in Berlin and in the Field with the V-EMulator at Vulcano, Italy — Preliminary Results [#2291]
Spectral characterization of volcanic rocks of Vulcano Island, using the spectral range of the Venus Emissivity Mapper (VEM)/VERITAS, in situ and in the DLR/PSL.
Adeli S.* Domac A. Mueller N. Nunes D. Garland S. P. et al.
Reykjanes Peninsula, Iceland, as an Analog Site for Venus; Remote Sensing Investigation and Planned Field Work to Support the VERITAS Mission [#2693]
Remote sensing, in-situ, and labratory investigation of Reykjanes lava fields, Iceland, as an analog site to Venus, in preparation for the VERITAS mission.
Vistica J. T.*
Leviathan: A Starship-Based Venus Aerobot for Low-Altitude and Surface Explorations [#1276]
The Leviathan Venus Explorer is a long-lived 30-ton nuclear-powered aerobot capable of landing and taking off almost anywhere while circumnavigating Venus.
Sur D.* Malaspina D.
Estimation of Double Layers and Phase-Space Holes at the Venus Magnetosphere During Its 4th Encounter with the Parker Solar Probe [#2113]
High-resolution Parker Solar Probe data is used to observe kinetic structures such as double layers, phase-space holes at the Venus induced magnetosphere.
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