Results 11 to 20 of about 67,700 (153)

Bulk and grain-scale minor sulfur isotope data reveal complexities in the dynamics of Earth's oxygenation. [PDF]

Proc Natl Acad Sci U S A, 2022
Izon G, Luo G, Uveges BT, Beukes N, Kitajima K, Ono S, Valley JW, Ma X, Summons RE.   +8 more
europepmc   +2 more sources

Large sulfur isotope fractionations in Martian sediments at Gale crater [PDF]

, 2017
Variability in the sulfur isotopic composition in sediments can reflect atmospheric, geologic and biological processes. Evidence for ancient fluvio-lacustrine environments at Gale crater on Mars and a lack of efficient crustal recycling mechanisms on the
AS Yen, C Freissinet, CK Shearer, DL Eldridge, DT Vaniman, F-Y Leung, GR Osinski, H Ohmoto, HB Franz, HB Franz, HB Franz, I Halevy, IN Bindeman, J Farquhar, J Farquhar, J Parnell, J Savarino, JP Greenwood, JP Greenwood, JP Greenwood, JP Grotzinger, KA Farley, KM Stack, M Nachon, O Abramov, RRI Seal, S Chakraborty, SA Benner, SP Schwenzer, SP Schwenzer, SS Johnson, T Ding   +31 more
core   +1 more source

Hartree-Fock-Bogoliubov Calculations in Coordinate Space: Neutron-Rich Sulfur, Zirconium, Cerium, and Samarium Isotopes [PDF]

, 2003
Using the Hartree-Fock-Bogoliubov (HFB) mean field theory in coordinate space, we investigate ground state properties of the sulfur isotopes from the line of stability up to the two-neutron dripline ($^{34-52}S$).
A. Blazkiewicz, A. S. Umar, A. S. Umar, A. S. Umar, E. Terán, E. Terán, J. C. Wells, V. E. Oberacker, V. E. Oberacker   +8 more
core   +1 more source

Calculations of Thermodynamic Sulfur Isotope Effect [PDF]

Journal of Nuclear Science and Technology, 1985
The isotopic reduced partition function ratios (RPFR), (s/s')f, for the 34S/32S isotopic pair were calculated for 24 sulfur compounds between 10 and 2,000K. Their magnitudes were in the following sequences; at low enough temperatures at which In(s/s')f depends only on the isotopic difference in frequency-sum, SF6>SO2F2>SF5Cl>SF5Br>SO4 2->SO2Cl2>SO3 ...
Takao OI, Naoko TAGUMA, Hidetake KAKIHANA   +2 more
openaire   +1 more source

Sclerite formation in the hydrothermal-vent “scaly-foot” gastropod — possible control of iron sulfide biomineralization by the animal [PDF]

, 2006
A gastropod from a deep-sea hydrothermal field at the Rodriguez triple junction, Indian Ocean, has scale-shaped structures, called sclerites, mineralized with iron sulfides on its foot.
Chiba, Hitoshi, Endo, Kazuyoshi, Hashimoto, Jun, Hirata, Takafumi, Horikoshi, Koki, Kato, Yasuhiro, Kirschvink, Joseph L., Kogure, Toshihiro, Kopp, Robert E., Mizota, Chitoshi, Nealson, Kenneth H., Ozaki, Noriaki, Suga, Akinobu, Suzuki, Yohey, Takai, Ken, Tsuchida, Shinji   +15 more
core   +2 more sources

Nature of Isomerism in Exotic Sulfur Isotopes [PDF]

Physical Review Letters, 2015
5 pages, 2 ...
Utsuno, Yutaka, Shimizu, Noritaka, Otsuka, Takaharu, Yoshida, Tooru, Tsunoda, Yusuke   +4 more
openaire   +3 more sources

Kinetic model of carbonate dissolution in Martian meteorite ALH84001 [PDF]

, 2003
The magnetites and sulfides located in the rims of carbonate globules in the Martian meteorite ALH84001 have been claimed as evidence of past life on Mars.
Humayun, Munir, Kopp, Robert E.
core   +1 more source

Sea-floor tectonics and submarine hydrothermal systems [PDF]

, 2005
The discovery of metal-depositing hot springs on the sea floor, and especially their link to chemosynthetic life, was among the most compelling and significant scientific advances of the twentieth century. More than 300 sites of hydrothermal activity and
de Ronde, Cornell D. J., Hannington, Mark D., Petersen, Sven   +2 more
core   +1 more source

Evidence for an impact-induced biosphere from the δ34S signature of sulphides in the Rochechouart impact structure, France [PDF]

, 2017
The highly eroded 23 km diameter Rochechouart impact structure, France, has extensive evidence for post-impact hydrothermal alteration and sulphide mineralization.
Boyce, A.J., Lambert, P., Lee, M.R., Lindgren, P., Simpson, S.L.   +4 more
core   +1 more source

Discovery of the Isotopes with 11 <= Z <= 19

, 2011
A total of 194 isotopes with 11 $\le$ Z $\le$ 19 have been identified to date. The discovery of these isotopes which includes the observation of unbound nuclei, is discussed.
Ajzenberg-Selove, Alvarez, Amaldi, Andersen, Artukh, Aston, Aston, Aston, Aston, Aston, Aston, Aston, Aston, Audi, Auger, Barton, Baumann, Benenson, Benenson, Benenson, Berg, Bethe, Birge, Boley, Bradner, Brosi, Butler, Cable, Cable, Cerny, Churchill, Cohen, Corson, Creutz, Curie, Curie, Dempster, Dempster, Détraz, Eckardt, Ellis, Fahlenbrach, Fermi, Frisch, Frisch, Ginepro, Glass, Goriely, Grahame, Grimm, Grévy, Guillemaud-Mueller, Guillemaud-Mueller, Hagberg, Hansen, Hardy, Hardy, Haslam, Hevesy, Hoag, Hollander, Huber, Huber, Huber, Huck, Hurst, Jelley, Joliot, Kashy, Katcoff, Kennedy, King, Klapisch, Klapisch, Klapisch, Kuerti, Kuroyanagi, Langevin, Langevin, Langevin, Larson, Lederer, Lewitowicz, Lindner, Lindner, Livingood, Lukyanov, M. Thoennessen, MacFarlane, Mantica, Marinov, McPherson, Meye, Miller, Morinaga, Morinaga, Morris, Mukha, Mulliken, Nethaway, Nier, Nier, Notani, Nurmia, Overstreet, Pollard, Pool, Reeder, Robertson, Robinson, Robinson, Robinson, Saint-Laurent, Sakurai, Sakurai, Seaborg, Seaborg, Sheline, Sheline, Snell, Strominger, Stähelin, Sun, Symons, Tarasov, Tarasov, Thoennessen, Turkevich, Tyren, Van Voorhis, Walke, Weimer, Westfall, White, White, Yaffe, Zeeman, Zerguerras, Zünti, Äystö   +139 more
core   +1 more source