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X-WR-CALNAME:CLEVER Planets
X-ORIGINAL-URL:https://cleverplanets.org
X-WR-CALDESC:Events for CLEVER Planets
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DTSTART:20180311T080000
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DTSTART:20190310T080000
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DTSTART:20200308T080000
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DTSTART:20201101T070000
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DTSTART:20211107T070000
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DTSTART:20221106T070000
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BEGIN:VEVENT
DTSTART;VALUE=DATE:20220307
DTEND;VALUE=DATE:20220312
DTSTAMP:20260423T191918
CREATED:20210831T214637Z
LAST-MODIFIED:20210831T214637Z
UID:2334-1646611200-1647043199@cleverplanets.org
SUMMARY:LPSC 2022
DESCRIPTION:
URL:https://cleverplanets.org/event/lpsc-2022/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20211213
DTEND;VALUE=DATE:20211218
DTSTAMP:20260423T191918
CREATED:20210831T214542Z
LAST-MODIFIED:20210831T214744Z
UID:2332-1639353600-1639785599@cleverplanets.org
SUMMARY:AGU 2021
DESCRIPTION:
URL:https://cleverplanets.org/event/agu-2021/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20200119
DTEND;VALUE=DATE:20200125
DTSTAMP:20260423T191918
CREATED:20190208T155029Z
LAST-MODIFIED:20190208T155029Z
UID:1644-1579392000-1579910399@cleverplanets.org
SUMMARY:2020 Gordon Research Conference - Origins of Life
DESCRIPTION:Information available – April 1\, 2019 \nApplication deadline – December 22\, 2019
URL:https://cleverplanets.org/event/2020-gordon-origins-life/
CATEGORIES:Conference
ATTACH;FMTTYPE=image/png:https://cleverplanets.org/wp-content/uploads/2019/02/grc_logo.png
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=America/Chicago:20191213T112000
DTEND;TZID=America/Chicago:20191213T233500
DTSTAMP:20260423T191918
CREATED:20191209T131816Z
LAST-MODIFIED:20191209T131835Z
UID:2124-1576236000-1576280100@cleverplanets.org
SUMMARY:Talk by Megan Duncan at AGU 2019
DESCRIPTION:San Francisco. \n“Variations in Moderately Volatile Elements in Planetary Bodies from Impact Vaporization” \nAbstract: \nPlanet-building processes have a strong effect on the distribution of the elements in the resulting bodies. In particular\, moderately volatile elements (MVEs) have distinct differences in depletion between the meteorite groups and the planets. Understanding the chemical effects of impacts and post-impact processes are necessary in order to place constraints on the bulk composition of the planet (pre-differentiation). Vaporizing collisions\, common in energetic periods of accretion such giant planet migration and the terrestrial giant impact stage\, can separate refractory and volatile components as the system re-equilibrates during vapor plume expansion and cooling. In order to understand the chemical changes caused by high velocity collisions\, we must know the liquid-vapor phase boundary of the dominant mineral(s) of the original bodies\, likely a silicate mineral such as olivine or pyroxene. To constrain the equations of state of these minerals\, we conducted shock-and-release experiments with the Sandia Z machine on single crystal forsterite\, olivine\, and bronzite to determine the pressure (P)\, temperature (T)\, entropy\, and density of the shocked and post-shocked states. \nUpon decompression from the shocked state\, the high pressure fluid intersects the phase boundary and separates into a two-phase mixture at high P and T (e.g.\, ~1–1000 bar and ~4000–6500 K)\, driving melt-vapor partitioning under near-equilibrium conditions with limited isotopic fractionation. As the system continues to cool\, the MVE concentrations evolve until the system reaches the triple point and the melt freezes. The remaining condensable vapor adsorbs onto the larger solid droplets or condenses as new dust. Thus\, the MVE concentrations in the post-impact system may have large variations that are correlated with particle size. We explore the hypothesis that impact vaporization leads to a net enrichment of MVEs in dust-sized particles. Nebular size-sorting processes may separate the larger\, MVE-poor solids and the MVE-rich dust\, creating zones of variable depletion. During accretion\, the MVE-enriched dust may be variably incorporated into planetesimals and contribute to the chemical diversity observed in meteorites and planets. \nSNL is managed by NTESS under DOE-NSSA contract DE-NA0003525.
URL:https://cleverplanets.org/event/talk-by-megan-duncan-at-agu-2019/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=America/Chicago:20191212T134000
DTEND;TZID=America/Chicago:20191212T180000
DTSTAMP:20260423T191918
CREATED:20191209T131315Z
LAST-MODIFIED:20191209T131315Z
UID:2120-1576158000-1576173600@cleverplanets.org
SUMMARY:Poster by Daman Grewal at AGU 2019
DESCRIPTION:San Francisco. \n“The core-mantle partitioning of carbon and nitrogen in carbon-undersaturated ultramafic systems” \nAbstract: \nIn addition to their highly volatile character\, segregation into the metallic core could have played an important role in explaining the depletion of carbon (C) and nitrogen (N) in the bulk silicate reservoirs of rocky bodies [e.g.\, 1\,2]. As the core-mantle partitioning character of C and N strongly depends on fO2\, they can act as a powerful tracers to understand the fO2-dependent volatile accretion history of terrestrial bodies. Previous high P-T experimental studies have shown that the highly siderophile character of C increases with decrease in fO2\, but can get suppressed in systems with high fH2\, while N acts as a siderophile element at >IW–2.5 and is lithophile at <IW–2.5 [3]. High P-T experiments on DCalloy/silicate and DNalloy/silicate published till date were conducted under graphite saturated conditions with basaltic to andesitic melt compositions primarily to quench glasses so that equilibrium C and N content in the silicate melts could be determined. However\, terrestrial Magma Oceans (MOs) are presumed to be C-undersaturated with ultramafic silicate melt compositions\, but such systems have not been simulated yet. \nHere we present 28 experiments in MgO capsules that yielded large silicate glass pools coexisting with quenched alloy melt. DCalloy/silicate and DNalloy/silicate were determined as function of fO2 (IW-7 to -1.5) at T=1600-1800 °C with nominally anhydrous (as low as 0.06 wt.% H2O) mafic-ultramafic silicate melts (NBO/T=0.6-3.2) at a fixed P (3 GPa). C and N in quenched metal and silicate products were measured using EPMA\, while C and H2O in silicate by SIMS. In contrast to previous studies our experiments show that the siderophile character of C can be much lower\, while N remains siderophile at even more reducing conditions (≥IW-4.5) primarily due to lower C content in the alloy relative to graphite saturated conditions. Our calculations predict that during core formation\, the siderophile character of C depends upon its activity in the metal\, while N can act as a siderophile element across the entire fO2 range relevant for terrestiral accretion; therefore\, bulk C content in the MOs\, in addition to fO2\, can strongly influence partitioning of C and N into the core forming alloys. \n[1] Dalou et al. (2017) EPSL [2] Grewal et al (2019) Sci. Adv. [3] Grewal et al (2019) GCA
URL:https://cleverplanets.org/event/poster-by-daman-grewal-at-agu-2019/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=America/Chicago:20191212T090000
DTEND;TZID=America/Chicago:20191212T091500
DTSTAMP:20260423T191918
CREATED:20191209T131008Z
LAST-MODIFIED:20191209T131008Z
UID:2117-1576141200-1576142100@cleverplanets.org
SUMMARY:Talk by James Eguchi at AGU Fall Meeting
DESCRIPTION:San Francisco. \n“Experimental investigation of a model ophicarbonate at deep subduction zone conditions – Implications for cycling of CO2 and H2O” \nAbstract: \nDue to their high CO2 and H2O contents\, and presence in both the mantle lithosphere1 as well as the mantle wedge2\, understanding the fate of ophicarbonates under subduction zone conditions is critical to understanding how these rocks may affect the deep H2O and C cycles3. However\, the fate of ophicarbonates during subduction has only been studied in the context of metamorphic devolatilization3 at shallow depths. \nHere\, we present results from an experimental phase relations study of a model ophicarbonate (SiO2 = 33.8 wt%\, MgO = 31.7 wt%\, CaO = 13.2 wt%\, CO2 = 8.7 wt%\, H2O = 4.2 wt% ) at 3-7 GPa and 700-1100 °C. We find that chlorite becomes unstable above 3 GPa and 800 °C. Under conditions above the breakdown of hydrous phases and below the solidus\, carbonates (magnesite + dolomite ≤ 4 GPa\, magnesite > 4 GPa) remain stable in equilibrium with an H2O-rich fluid. Above the solidus (between 800-850 °C from 3-7 GPa)\, carbonates remain stable along with silicate minerals (cpx\, olivine\, garnet) and a CO2-rich melt phase over a restricted temperature interval until carbonates are completely melted out at T > 1000 °C at 3-5 GPa and > 1100 °C at 7 GPa. \nDue to the breakdown of chlorite at conditions above 3 GPa and 800 °C our experiments suggest that ophicarbonates will be nearly completely dehydrated at subarc depths\, delivering H2O to arc magma source regions. The stability of carbonates in our experiments suggest that even for the hottest subduction zones\, ophicarbonates in the mantle lithosphere (below slab MOHO) can retain C in the form of crystalline carbonates past subarc depths and deliver C deeper into the mantle. If ophicarbonates formed in the mantle wedge become mechanically coupled with the subducting slab\, then C can be completely released in the hottest subduction zones in the form of CO2-rich melts\, while ophicarbonates in cooler subduction zones may retain some C. In agreement with previous modeling studies3\, the present experimental study suggests that ophicarbonates dehydrate and deliver H2O to arc magma source regions and retain some amount of C in all but the hottest subduction zones\, highlighting the importance of these lithologies in delivering C past subarc depths deep into the mantle. \n1Alt\, J. C. et al. Lithos (2013) \n2Sieber\, M. J. et al. EPSL (201) \n3Kerrick\, D. M.\, & Connolly\, J. A. D. Geology (1998)
URL:https://cleverplanets.org/event/talk-by-james-eguchi-at-agu-fall-meeting/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=America/Chicago:20191209T082500
DTEND;TZID=America/Chicago:20191209T083000
DTSTAMP:20260423T191918
CREATED:20191209T131559Z
LAST-MODIFIED:20191209T132313Z
UID:2122-1575879900-1575880200@cleverplanets.org
SUMMARY:Talk by Sarah Stewart at AGU 2019
DESCRIPTION:San Francisco. \n“Expect more surprises during planet formation” \nAbstract: \nPlanet assembly drives materials into pressure-temperature regimes far beyond the current states of planetary objects in our solar system. As a result\, planet formation produces unfamiliar phenomena\, such impact-generated vapor bubbles in the solar nebula and fast-spinning synestias. These newly recognized phenomena lead to fresh views on how to use geochemical observations to reconstruct planet formation.
URL:https://cleverplanets.org/event/talk-by-sarah-stewart-at-agu-2019/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20190715
DTEND;VALUE=DATE:20190720
DTSTAMP:20260423T191918
CREATED:20190208T154256Z
LAST-MODIFIED:20190208T154438Z
UID:1637-1563148800-1563580799@cleverplanets.org
SUMMARY:2019 Sagan Exoplanet Summer Workshop - Astrobiology for Astronomers
DESCRIPTION:2019 Sagan Exoplanet Summer Workshop – Astrobiology for Astronomers\nHOSTED BY THE NASA EXOPLANET SCIENCE INSTITUTE\, HAMEETMAN AUDITORIUM\, CAHILL BUILDING\, CALIFORNIA INSTITUTE OF TECHNOLOGY\, PASADENA\, CA\nSubmit talks/posters – May 9- June 28\nFREE to register – deadline May 16
URL:https://cleverplanets.org/event/2019-sagan-exoplanet-workshop/
CATEGORIES:Conference
ATTACH;FMTTYPE=image/jpeg:https://cleverplanets.org/wp-content/uploads/2019/02/exo.jpg
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20190623
DTEND;VALUE=DATE:20190629
DTSTAMP:20260423T191918
CREATED:20190208T154733Z
LAST-MODIFIED:20190208T154812Z
UID:1640-1561248000-1561766399@cleverplanets.org
SUMMARY:2019 Gordon Research Conference - Origins of Solar Systems
DESCRIPTION:Meteoritical\, Spacecraft and Astrophysical Perspectives on the Assembly and Composition of Planets\nHosted at Mount Holyoke College\, 50 College Street\, South Hadley\, MA\, US \nThe Gordon Research Conference on Origins of Solar Systems brings together a diverse group of scientists to discuss research at the frontier of understanding how planets and planetary systems form. Invited speakers from the fields of astronomy\, astrophysics\, cosmochemistry\, and planetary science will present their latest findings. A particular focus at this meeting will be the latest results from the Hayabusa2\, Osiris-Rex\, and New Horizons missions to primitive solar system bodies\, exoplanet results from the TESS space telescope\, and results from ground-based astronomical facilities like the Atacama Large Millimeter Array.\nApplication deadline – May 26\, 2019
URL:https://cleverplanets.org/event/2019-gordon-origins-solar-systems/
CATEGORIES:Conference
ATTACH;FMTTYPE=image/png:https://cleverplanets.org/wp-content/uploads/2019/02/grc_logo.png
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20190318
DTEND;VALUE=DATE:20190323
DTSTAMP:20260423T191918
CREATED:20180824T145209Z
LAST-MODIFIED:20190129T145259Z
UID:999-1552867200-1553299199@cleverplanets.org
SUMMARY:LPSC
DESCRIPTION:50th annual Lunar and Planetary Science Conference\, bringing together “international specialists in petrology\, geochemistry\, geophysics\, geology\, and astronomy to present the latest results of research in planetary science\,” Houston\, TX \nAbstract deadline – January 9\, 2019\nProgram available – February 1\, 2019 \n 
URL:https://cleverplanets.org/event/lpsc/
CATEGORIES:Conference
ATTACH;FMTTYPE=image/png:https://cleverplanets.org/wp-content/uploads/2018/08/LPSC2019home-graphic.png
END:VEVENT
BEGIN:VEVENT
DTSTART;TZID=America/Chicago:20190115T080000
DTEND;TZID=America/Chicago:20190116T120000
DTSTAMP:20260423T191918
CREATED:20190112T000832Z
LAST-MODIFIED:20190112T001721Z
UID:1572-1547539200-1547640000@cleverplanets.org
SUMMARY:Kick-Off Meeting
DESCRIPTION:The first meeting of CLEVER Planets attendees is happening January 14-15th\, 2019\, at Rice University in Houston\, TX. At this Kick-Off Meeting\, co-investigators\, collaborators and their postdoctoral scholars and students will convene to share their research and discuss goals and collaborations for the project over the next few years. \nSee the itinerary and list of attendees here:\nCLEVERPlanets_Kick-OffMeeting_Schedule
URL:https://cleverplanets.org/event/kick-off-meeting/
CATEGORIES:CLEVERPlanet Event,Conference,Meeting
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20181210
DTEND;VALUE=DATE:20181215
DTSTAMP:20260423T191918
CREATED:20180824T145012Z
LAST-MODIFIED:20190129T145307Z
UID:996-1544400000-1544831999@cleverplanets.org
SUMMARY:AGU Meeting
DESCRIPTION:American Geophysical Union’s Annual Fall Meeting\, Washington\, D.C.
URL:https://cleverplanets.org/event/agu-meeting/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20181104
DTEND;VALUE=DATE:20181108
DTSTAMP:20260423T191918
CREATED:20180824T144234Z
LAST-MODIFIED:20190129T145318Z
UID:990-1541289600-1541635199@cleverplanets.org
SUMMARY:GSA Meeting
DESCRIPTION:Annual Geological Society of America Meeting\, Indianapolis\, Indiana
URL:https://cleverplanets.org/event/gsa-meeting/
CATEGORIES:Conference
END:VEVENT
BEGIN:VEVENT
DTSTART;VALUE=DATE:20180924
DTEND;VALUE=DATE:20180929
DTSTAMP:20260423T191918
CREATED:20180824T150335Z
LAST-MODIFIED:20190129T145327Z
UID:1004-1537747200-1538179199@cleverplanets.org
SUMMARY:EANA Meeting
DESCRIPTION:European Astrobiology Conference\, Berlin\, Germany
URL:https://cleverplanets.org/event/eana-meeting/
CATEGORIES:Conference
END:VEVENT
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