Abstract is: Sanjeev Gupta is professor of Earth Science at Imperial College London. Gupta is part of the NASA Mars Science mission, particularly the Curiosity rover mission currently exploring Gale Crater.
| human | Q5 |
| P2888 | exact match | https://www.imperial.ac.uk/people/s.gupta |
| P2671 | Google Knowledge Graph ID | /g/11f32wgxy2 |
| P269 | IdRef ID | 158130448 |
| P496 | ORCID iD | 0000-0001-6415-1332 |
| P2038 | ResearchGate profile ID | Sanjeev-Gupta-36 |
| P214 | VIAF ID | 286324287 |
| P108 | employer | Imperial College London | Q189022 |
| P734 | family name | Gupta | Q3632770 |
| Gupta | Q3632770 | ||
| Gupta | Q3632770 | ||
| P101 | field of work | earth science | Q8008 |
| planetary science | Q104499 | ||
| P735 | given name | Sanjeev | Q98827205 |
| Sanjeev | Q98827205 | ||
| P106 | occupation | geologist | Q520549 |
| university teacher | Q1622272 | ||
| P21 | sex or gender | male | Q6581097 |
| Q90620629 | A Diverse Array of Fluvial Depositional Systems in Arabia Terra: Evidence for mid-Noachian to Early Hesperian Rivers on Mars |
| Q22065596 | A Habitable Fluvio-Lacustrine Environment at Yellowknife Bay, Gale Crater, Mars |
| Q104154226 | A Lacustrine Paleoenvironment Recorded at Vera Rubin Ridge, Gale Crater: Overview of the Sedimentology and Stratigraphy Observed by the Mars Science Laboratory Curiosity Rover |
| Q106705194 | A Rock Record of Complex Aeolian Bedforms in a Hesperian Desert Landscape: The Stimson Formation as Exposed in the Murray Buttes, Gale Crater, Mars |
| Q57868345 | A background to Mars exploration and research |
| Q104154227 | A lacustrine paleoenvironment recorded at Vera Rubin ridge, Gale crater: Overview of the sedimentology and stratigraphy observed by the Mars Science Laboratory Curiosity rover |
| Q108865612 | A record of syn-tectonic sedimentation revealed by perched alluvial fan deposits in Valles Marineris, Mars |
| Q115484806 | Alteration history of Séítah formation rocks inferred by PIXL x-ray fluorescence, x-ray diffraction, and multispectral imaging on Mars |
| Q113645069 | An olivine cumulate outcrop on the floor of Jezero crater, Mars |
| Q56594514 | Ancient Martian aeolian processes and palaeomorphology reconstructed from the Stimson formation on the lower slope of Aeolis Mons, Gale crater, Mars |
| Q113620969 | Ancient Winds, Waves, and Atmosphere in Gale Crater, Mars, Inferred From Sedimentary Structures and Wave Modeling |
| Q113644964 | Aqueously altered igneous rocks sampled on the floor of Jezero crater, Mars |
| Q105126332 | Aram Dorsum: An Extensive Mid‐Noachian Age Fluvial Depositional System in Arabia Terra, Mars |
| Q125868605 | Architecture of fluvial and deltaic deposits exposed along the eastern edge of Jezero crater western fan |
| Q107492651 | Billion-year exposure ages in Gale crater (Mars) indicate Mount Sharp formed before the Amazonian period |
| Q127506885 | Burial and Exhumation of Sedimentary Rocks Revealed by the Base Stimson Erosional Unconformity, Gale Crater, Mars |
| Q59914883 | Calibrating Mars Orbiter Laser Altimeter pulse widths at Mars Science Laboratory candidate landing sites |
| Q66314537 | Candidate Desiccation Cracks in the Upper Murray Formation, Gale Crater, Mars |
| Q28236944 | Catastrophic flooding origin of shelf valley systems in the English Channel |
| Q59762232 | ChemCam results from the Shaler outcrop in Gale crater, Mars |
| Q57874207 | Chemical variations in Yellowknife Bay formation sedimentary rocks analyzed by ChemCam on board the Curiosity rover on Mars |
| Q55347021 | Clay mineral diversity and abundance in sedimentary rocks of Gale crater, Mars. |
| Q60418904 | Comments and Reply on "Mesozoic overthrust tectonics in south China" |
| Q57865654 | Comparing orbiter and rover image-based mapping of an ancient sedimentary environment, Aeolis Palus, Gale crater, Mars |
| Q123467525 | Compositionally and density stratified igneous terrain in Jezero crater, Mars |
| Q104697592 | Constraints on the origin and evolution of Iani Chaos, Mars |
| Q104697608 | Correction to “Late Noachian to Hesperian climate change on Mars: Evidence of episodic warming from transient crater lakes near Ares Vallis” |
| Q34497447 | Deposition, exhumation, and paleoclimate of an ancient lake deposit, Gale crater, Mars |
| Q57967640 | Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater |
| Q57867905 | Diagenetic silica enrichment and late-stage groundwater activity in Gale crater, Mars |
| Q66363722 | Discovery of silica‐rich lacustrine and eolian sedimentary rocks in Gale Crater, Mars |
| Q57660868 | Discussion on ‘Tectonic and environmental controls on Palaeozoic fluvial environments: reassessing the impacts of early land plants on sedimentation’ |
| Q57847757 | Does slab-window opening cause uplift of the overriding plate? A case study from the Gulf of California |
| Q34390881 | Elemental geochemistry of sedimentary rocks at Yellowknife Bay, Gale crater, Mars |
| Q59831224 | Encounters with an unearthly mudstone: Understanding the first mudstone found on Mars |
| Q57868145 | Episodic and Declining Fluvial Processes in Southwest Melas Chasma, Valles Marineris, Mars |
| Q117990083 | Evidence for Fluctuating Wind in Shaping an Ancient Martian Dune Field: The Stimson Formation at the Greenheugh Pediment, Gale Crater |
| Q100249762 | Evidence for a Diagenetic Origin of Vera Rubin Ridge, Gale Crater, Mars: Summary and Synthesis of Curiosity's Exploration Campaign |
| Q61999784 | Evidence for plunging river plume deposits in the Pahrump Hills member of the Murray formation, Gale crater, Mars |
| Q127506909 | Evolution of a Lake Margin Recorded in the Sutton Island Member of the Murray Formation, Gale Crater, Mars |
| Q57868269 | Extensive Noachian fluvial systems in Arabia Terra: Implications for early Martian climate |
| Q104218359 | Extraformational sediment recycling on Mars |
| Q127661882 | Facies architecture of a net transgressive sandstone reservoir analog: The Cretaceous Hosta Tongue, New Mexico |
| Q58081182 | Fill and spill of giant lakes in the eastern Valles Marineris region of Mars |
| Q61847347 | Flow processes and sedimentation in submarine channel bends |
| Q59914902 | Formation of an Hesperian-aged sedimentary basin containing phyllosilicates in Coprates Catena, Mars |
| Q123467546 | From Lake to River: Documenting an Environmental Transition Across the Jura/Knockfarril Hill Members Boundary in the Glen Torridon Region of Gale Crater (Mars) |
| Q59708101 | Geologic overview of the Mars Science Laboratory rover mission at the Kimberley, Gale crater, Mars |
| Q120514603 | Geological, multispectral, and meteorological imaging results from the Mars 2020 Perseverance rover in Jezero crater |
| Q120518203 | Geology and Stratigraphic Correlation of the Murray and Carolyn Shoemaker Formations Across the Glen Torridon Region, Gale Crater, Mars |
| Q104218363 | Grain Size Variations in the Murray Formation: Stratigraphic Evidence for Changing Depositional Environments in Gale Crater, Mars |
| Q56546877 | Hesperian equatorial thermokarst lakes in Ares Vallis as evidence for transient warm conditions on Mars |
| Q104697572 | Hydraulic modeling of a distributary channel of Athabasca Valles, Mars, using a high-resolution digital terrain model |
| Q127469086 | Ice? Salt? Pressure? Sediment deformation structures as evidence of late-stage shallow groundwater in Gale crater, Mars |
| Q34390874 | In situ radiometric and exposure age dating of the martian surface |
| Q120518107 | Influence of fault-controlled topography on fluvio-deltaic sedimentary systems in Eberswalde crater, Mars |
| Q57409447 | Instrumentation Development for In Situ 40 Ar/39 Ar Planetary Geochronology |
| Q28294794 | Isotope ratios of H, C, and O in CO2 and H2O of the martian atmosphere |
| Q107790727 | Landscape evolution at extensional relay zones |
| Q38379409 | Large wind ripples on Mars: A record of atmospheric evolution |
| Q104697661 | Late Noachian to Hesperian climate change on Mars: Evidence of episodic warming from transient crater lakes near Ares Vallis |
| Q106500477 | Mars 2020 science team assessment of Jezero crater |
| Q106575376 | Mars Hand Lens Imager (MAHLI) Efforts and Observations at the Rocknest Eolian Sand Shadow in Curiosity's Gale Crater Field Site |
| Q38465063 | Mars sedimentary geology: key concepts and outstanding questions |
| Q34347765 | Martian fluvial conglomerates at Gale crater |
| Q34390861 | Mineralogy of a mudstone at Yellowknife Bay, Gale crater, Mars |
| Q57852716 | Mineralogy of an ancient lacustrine mudstone succession from the Murray formation, Gale crater, Mars |
| Q28834159 | Mineralogy, provenance, and diagenesis of a potassic basaltic sandstone on Mars: CheMin X-ray diffraction of the Windjana sample (Kimberley area, Gale Crater) |
| Q59914879 | Minimum effective area for high resolution crater counting of martian terrains |
| Q104697546 | Multi-resolution digital terrain models and their potential for Mars landing site assessments |
| Q55870259 | Organic matter preserved in 3-billion-year-old mudstones at Gale crater, Mars |
| Q123469759 | Overview and Results From the Mars 2020 Perseverance Rover's First Science Campaign on the Jezero Crater Floor |
| Q57727560 | Overview of the Mars Science Laboratory mission: Bradbury Landing to Yellowknife Bay and beyond |
| Q104747888 | Oxia Planum: The Landing Site for the ExoMars "Rosalind Franklin" Rover Mission: Geological Context and Prelanding Interpretation |
| Q109947395 | Perseverance rover reveals an ancient delta-lake system and flood deposits at Jezero crater, Mars |
| Q104220491 | Photogeologic Map of the Perseverance Rover Field Site in Jezero Crater Constructed by the Mars 2020 Science Team |
| Q127661643 | Preserved Stratigraphic Architecture and Evolution of A Net-Transgressive Mixed Wave- and Tide-Influenced Coastal System: The Cliff House Sandstone, Northwestern New Mexico, U.S.A |
| Q57537423 | Quantifying geological processes on Mars—Results of the high resolution stereo camera (HRSC) on Mars express |
| Q36390087 | Redox stratification of an ancient lake in Gale crater, Mars. |
| Q58083356 | Retreat of a giant cataract in a long-lived (3.7–2.6 Ga) martian outflow channel |
| Q57603852 | Rift flank uplift at the Gulf of California: No requirement for asthenospheric upwelling |
| Q52677961 | Sedimentary processes of the Bagnold Dunes: Implications for the eolian rock record of Mars. |
| Q127506884 | Sedimentological and Geochemical Perspectives on a Marginal Lake Environment Recorded in the Hartmann's Valley and Karasburg Members of the Murray Formation, Gale Crater, Mars |
| Q66314517 | Sedimentology and Stratigraphy of the Murray Formation, Gale Crater, Mars |
| Q56594513 | Shaler: in situ analysis of a fluvial sedimentary deposit on Mars |
| Q57455465 | Stepped fans and facies-equivalent phyllosilicates in Coprates Catena, Mars |
| Q123473408 | Stratigraphic Relationships in Jezero Crater, Mars: Constraints on the Timing of Fluvial‐Lacustrine Activity From Orbital Observations |
| Q66720775 | Stratigraphy and Sedimentology of the Murray Formation, as observed using the Mars Science Laboratory Curiosity Rover |
| Q57868191 | Surface-based 3D measurements of small aeolian bedforms on Mars and implications for estimating ExoMars rover traversability hazards |
| Q114589177 | Tectonic significance of Cenozoic exhumation and foreland basin evolution in the Western Alps |
| Q59747107 | The 2016 UK Space Agency Mars Utah Rover Field Investigation (MURFI) |
| Q100233498 | The Chemostratigraphy of the Murray Formation and Role of Diagenesis at Vera Rubin Ridge in Gale Crater, Mars, as Observed by the ChemCam Instrument |
| Q57868152 | The Hypanis Valles delta: The last highstand of a sea on early Mars? |
| Q127471520 | The Origin of the Fracture Networks in the Mudstones of Gale Crater Mars; Their Implications Regarding the State of Stress and Fluid Pressure During Their Formation and the Depth to Which They Were Buried |
| Q45796785 | The PanCam Instrument for the ExoMars Rover |
| Q59781674 | The Sedimentary Record of Mars |
| Q66360591 | The Stimson Formation: Determining the Morphology of a Dry Aeolian Dune System and its Climatic Significance in Gale Crater, Mars |
| Q61847340 | The influence of bend amplitude and planform morphology on flow and sedimentation in submarine channels |
| Q104218423 | The internal sedimentary architecture of Terrestrial sinuous ridges: clues to understanding sinuous ridges on Mars |
| Q59781672 | The origin and evolution of the Peace Vallis fan system that drains to the Curiosity landing area, Gale Crater, Mars |
| Q59783848 | The potassic sedimentary rocks in Gale Crater, Mars, as seen by ChemCam on board Curiosity |
| Q29167330 | Two-stage opening of the Dover Strait and the origin of island Britain |
| Q59746174 | Using bathymetry to identify basin inversion structures on the English Channel shelf |
| Q34390894 | Volatile and organic compositions of sedimentary rocks in Yellowknife Bay, Gale crater, Mars |
| Q34373730 | Volatile, isotope, and organic analysis of martian fines with the Mars Curiosity rover |
| Q58457962 | What sets topographic relief in extensional footwalls? |