Search Results - Planet Earth III

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    A giant planet beyond the snow line in microlensing event OGLE-2011-BLG-0251 by Kains, N., Street, R., Choi, J., Han, C., Udalski, A., Almeida, L., Jablonski, F., Tristram, P., Jorgensen, U., Szymanski, M., Kubiak, M., Pietrzynski, G., Soszynski, I., Poleski, R., Kozlowski, S., Pietrukowicz, P., Ulaczyk, K., Wyrzykowski, L., Skowron, J., Alsubai, K., Bozza, V., Browne, P., Burgdorf, M., Calchi Novati, S., Dodds, P., Dominik, M., Dreizler, S., Fang, X., Grundahl, F., Gu, C., Hardis, S., Harpsoe, K., Hessman, F., Hinse, T., Hornstrup, A., Hundertmark, M., Jessen-Hansen, J., Kerins, E., Liebig, C., Lund, M., Lundkvist, M., Mancini, L., Mathiasen, M., Penny, M., Rahvar, S., Ricci, D., Sahu, K., Scarpetta, G., Skottfelt, J., Snodgrass, C., Southworth, J., Surdej, J., Tregloan-Reed, J., Wambsganss, J., Wertz, O., Bajek, D., Bramich, D., Horne, K., Ipatov, S., Steele, I., Tsapras, Y., Abe, F., Bennett, D., Bond, I., Botzler, C., Chote, P., Freeman, M., Fukui, A., Furusawa, K., Itow, Y., Ling, C., Masuda, K., Matsubara, Y., Miyake, N., Muraki, Y., Ohnishi, K., Rattenbury, N., Saito, T., Sullivan, D., Sumi, T., Suzuki, D., Suzuki, K., Sweatman, W., Takino, S., Wada, K., Yock, P., Allen, W., Batista, V., Chung, S., Christie, G., DePoy, D., Drummond, J., Gaudi, B., Gould, A., Henderson, C., Jung, Y., Koo, J., Lee, C., McCormick, J., McGregor, D., Munoz, J., Natusch, T., Ngan, H., Park, H., Pogge, R., Shin, I., Yee, J., Albrow, M., Bachelet, E., Beaulieu, J., Brillant, S., Caldwell, J., Cassan, A., Cole, A., Corrales, E., Coutures, C., Dieters, S., Dominis Prester, D., Donatowicz, J., Fouque, P., Greenhill, J., Kane, S., Kubas, D., Marquette, J., Martin, R., Meintjes, P., Menzies, J., Pollard, K., Williams, Andrew, Wouters, D., Zub, M.

    Published 2013
    “…Based on detailed modelling of the observed light curve, we find that the lens is composed of twomasses with a mass ratio q = 1.9 × 10-3. Thanks to our detection of higher-order effects on the light curve due to the Earth’s orbital motion and the finite size of source, we are able to measure the mass and distance to the lens unambiguously.Results. …”
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    Origin and age of the earliest Martian crust from meteorite NWA 7533 by Humayun, M., Nemchin, Alexander, Zanda, B., Hewins, R., Grange, Marion, Kennedy, Allen, Lorand, J., Gopel, C., Fieni, C., Pont, S., Deldicque, D.

    Published 2013
    “…The ancient cratered terrain of the southern highlands of Mars is thought to hold clues to the planet’s early differentiation [1,2] but until now no meteoritic regolith breccias have been recovered from Mars. …”
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    Pb isotope insight into the formation of the Earth's first stable continents by Hartnady, Michael, Kirkland, Christopher, Smithies, R. Hugh, Johnson, S.P., Johnson, Tim

    Published 2022
    “…The formation of stable buoyant continental crust during the Archaean Eon was fundamental in establishing the planet's geochemical reservoirs. However, the processes that created Earth's first continents and the timescales over which they formed are debated. …”
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    Bimodality in zircon oxygen isotopes and implications for crustal melting on the early Earth by Kirkland, Chris, Johnson, Tim, Gillespie, Jack, Martin, L., Rankenburg, Kai, Kaempf, Jonas, Clark, Chris

    Published 2024
    “…Zircons from the oldest dated felsic crust, the Acasta Gneiss Complex, Canada, provide key information that may help understand the generation of crust on our nascent planet. When screened to eliminate grains with secondary alteration by measuring relative hydration (Δ16O1H/16O), primary ≥ 3.99 Ga zircon cores show δ18O of 5.88 ± 0.15 ‰, at the extreme upper (heavy) range for mantle values. …”
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    MarcoPolo-R near earth asteroid sample return mission by Barucci, M., Cheng, A., Michel, P., Benner, L., Binzel, R., Bland, Phil, Böhnhardt, H., Brucato, J., Campo Bagatin, A., Cerroni, P., Dotto, E., Fitzsimmons, A., Franchi, I., Green, S., Lara, L., Licandro, J., Marty, B., Muinonen, K., Nathues, A., Oberst, J., Rivkin, A., Robert, F., Saladino, R., Trigo-Rodriguez, J., Ulamec, S., Zolensky, M.

    Published 2012
    “…MarcoPolo-R takes advantage of three industrial studies completed as part of the previous Marco Polo mission (see ESA/SRE (2009)3, Marco Polo Yellow Book) and of the expertise of the consortium led by Dr. …”
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    Has the impact flux of small and large asteroids varied through time on Mars, the Earth and the Moon? by Lagain, Anthony, Kreslavsky, M., Baratoux, D., Liu, Yebo, Devillepoix, Hadrien, Bland, Philip, Benedix, Gretchen, Doucet, Luc, Servis, K.

    Published 2022
    “…However, asteroid break-up events in the main belt may have been responsible for cratering spikes over the last ∼2 Ga on the Earth-Moon system. Due to its proximity with the main asteroid belt, i.e., the main impactors reservoir, Mars is at the outpost of these events with respect to the other inner planets. …”
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    The global lead isotope system: Toward a new framework reflecting Earth's dynamic evolution by Doucet, Luc, Li, Zheng-Xiang, Fougerouse, Denis, Olierook, Hugo, Gamaleldien, Hamed, Kirkland, Chris, Hartnady, Michael

    Published 2023
    “…However, the Pb isotope systematics of the Earth are subject to two major paradoxes. Assuming our planet evolved uniformly from a chondritic composition, all the present-day Earth chemical reservoirs should plot on the 4.55 Ga meteorite isochron, also known as the geochron; but in fact, all known reservoirs are more radiogenic (having excess 206Pb and 207Pb) than the carbonaceous chondrites, constituting the first Pb paradox. …”
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    Intercalibration of the Hb3gr 40Ar/39Ar dating standard. by Jourdan, Fred, Verati, C., Feraud, G.

    Published 2006
    “…This age is indistinguishable within uncertainty from the K/Ar age previously reported at 1072 11 Ma [Turner G., Huneke, J.C., Podosek, F.A., Wasserburg, G.J., 1971. 40Ar-39Ar ages and cosmic ray exposure ages of Apollo 14 samples. Earth Planet. Sci. Lett. 12, 19-35]. The R-value determined in this study can also be used to intercalibrate FCs if we consider the K/Ar date of 1072 Ma as a reference age for Hb3gr. …”
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    Oxygen isotopes in Pilbara Craton zircons support a global increase in crustal recycling at 3.2Ga by Van Kranendonk, M., Kirkland, Chris, Cliff, J.

    Published 2015
    “…These results align with global datasets of oxygen isotopes, and point to a more general change in the geodynamics of Earth associated with the secular decrease in heat output of our planet.…”
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    Lingua revolution and human civilization (special Season) by Yaacob, Solehah@Nik Najah Fadilah

    Published 2016
    “…After the mega explosion of the Big Bang, the planet Earth became divided into two parts, namely the earth’s surface and the sky, each of which is composed of seven layers (as mentioned in the Quran, Torah and Gospel). …”
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    Attend to other water woes, too by Abd Razak, Dzulkifli

    Published 2005
    “…With the tsunami tragedy still fresh in our minds, perhaps many would be curious to know how much water there is on Earth. According to the National Geographic (Sept, 2002), if the Earth crust is smothered, the entire surface of the planet would be covered by 2682.24 metres of seawater. …”
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    International law of the sea by Eishan Jan, Mohammad Naqib

    Published 2016
    “…This paper discusses an important aspect of public international law that governs the vast oceans of the world, covering three fourths of the planet earth. It explains the the natural resources of the seas, ships that are sailing on the seas and protection and preservation of the marine environment.…”
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    A study of the relationship between solar activities and earthquakes / Indriani Sukma by Indriani , Sukma

    Published 2017
    “…The Sun is a prime source of energy while the Earth is the third planet near to the Sun and the only planet that has very large seismic activity. …”
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    Energy Efficient Process, Dynamic Modelling and Control of Boric Acid Promoted Potassium Carbonate Based CO2 Capture System by Ayittey, Foster Kofi

    Published 2020
    “…Planet earth is warming up, and anthropogenic emission of CO2 is acknowledged as a principal contributing factor. …”
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