Zobrazeno 1 - 10
of 36
pro vyhledávání: '"R J Bodnar"'
Autor:
R. Esposito, D. Redi, L. V. Danyushevsky, A. Gurenko, B. De Vivo, C. E. Manning, R. J. Bodnar, M. Steele-MacInnis, M.-L. Frezzotti
Publikováno v:
European Journal of Mineralogy, Vol 35, Pp 921-948 (2023)
Mount Somma–Vesuvius is a stratovolcano that represents a geological hazard to the population of the city of Naples and surrounding towns in southern Italy. Historically, volcanic eruptions at Mt. Somma–Vesuvius (SV) include high-magnitude Plinia
Externí odkaz:
https://doaj.org/article/195e668e017049ad8f8cf425984a2480
Publikováno v:
Geofluids, Vol 2021 (2021)
Several recent models that have been put forth to explain bradyseism at Campi Flegrei (CF), Italy, are discussed. Data obtained during long-term monitoring of the CF volcanic district has led to the development of a model based on lithological-struct
Externí odkaz:
https://doaj.org/article/f71bd2bb21224a9fb0cd496d8e613e3d
Autor:
T. Nakamura, M. Matsumoto, K. Amano, Y. Enokido, M. E. Zolensky, T. Mikouchi, H. Genda, S. Tanaka, M. Y. Zolotov, K. Kurosawa, S. Wakita, R. Hyodo, H. Nagano, D. Nakashima, Y. Takahashi, Y. Fujioka, M. Kikuiri, E. Kagawa, M. Matsuoka, A. J. Brearley, A. Tsuchiyama, M. Uesugi, J. Matsuno, Y. Kimura, M. Sato, R. E. Milliken, E. Tatsumi, S. Sugita, T. Hiroi, K. Kitazato, D. Brownlee, D. J. Joswiak, M. Takahashi, K. Ninomiya, T. Takahashi, T. Osawa, K. Terada, F. E. Brenker, B. J. Tkalcec, L. Vincze, R. Brunetto, A. Aléon-Toppani, Q. H. S. Chan, M. Roskosz, J.-C. Viennet, P. Beck, E. E. Alp, T. Michikami, Y. Nagaashi, T. Tsuji, Y. Ino, J. Martinez, J. Han, A. Dolocan, R. J. Bodnar, M. Tanaka, H. Yoshida, K. Sugiyama, A. J. King, K. Fukushi, H. Suga, S. Yamashita, T. Kawai, K. Inoue, A. Nakato, T. Noguchi, F. Vilas, A. R. Hendrix, C. Jaramillo-Correa, D. L. Domingue, G. Dominguez, Z. Gainsforth, C. Engrand, J. Duprat, S. S. Russell, E. Bonato, C. Ma, T. Kawamoto, T. Wada, S. Watanabe, R. Endo, S. Enju, L. Riu, S. Rubino, P. Tack, S. Takeshita, Y. Takeichi, A. Takeuchi, A. Takigawa, D. Takir, T. Tanigaki, A. Taniguchi, K. Tsukamoto, T. Yagi, S. Yamada, K. Yamamoto, Y. Yamashita, M. Yasutake, K. Uesugi, I. Umegaki, I. Chiu, T. Ishizaki, S. Okumura, E. Palomba, C. Pilorget, S. M. Potin, A. Alasli, S. Anada, Y. Araki, N. Sakatani, C. Schultz, O. Sekizawa, S. D. Sitzman, K. Sugiura, M. Sun, E. Dartois, E. De Pauw, Z. Dionnet, Z. Djouadi, G. Falkenberg, R. Fujita, T. Fukuma, I. R. Gearba, K. Hagiya, M. Y. Hu, T. Kato, T. Kawamura, M. Kimura, M. K. Kubo, F. Langenhorst, C. Lantz, B. Lavina, M. Lindner, J. Zhao, B. Vekemans, D. Baklouti, B. Bazi, F. Borondics, S. Nagasawa, G. Nishiyama, K. Nitta, J. Mathurin, T. Matsumoto, I. Mitsukawa, H. Miura, A. Miyake, Y. Miyake, H. Yurimoto, R. Okazaki, H. Yabuta, H. Naraoka, K. Sakamoto, S. Tachibana, H. C. Connolly, D. S. Lauretta, M. Yoshitake, M. Yoshikawa, K. Yoshikawa, K. Yoshihara, Y. Yokota, K. Yogata, H. Yano, Y. Yamamoto, D. Yamamoto, M. Yamada, T. Yamada, T. Yada, K. Wada, T. Usui, R. Tsukizaki, F. Terui, H. Takeuchi, Y. Takei, A. Iwamae, H. Soejima, K. Shirai, Y. Shimaki, H. Senshu, H. Sawada, T. Saiki, M. Ozaki, G. Ono, T. Okada, N. Ogawa, K. Ogawa, R. Noguchi, H. Noda, M. Nishimura, N. Namiki, S. Nakazawa, T. Morota, A. Miyazaki, A. Miura, Y. Mimasu, K. Matsumoto, K. Kumagai, T. Kouyama, S. Kikuchi, K. Kawahara, S. Kameda, T. Iwata, Y. Ishihara, M. Ishiguro, H. Ikeda, S. Hosoda, R. Honda, C. Honda, Y. Hitomi, N. Hirata, T. Hayashi, M. Hayakawa, K. Hatakeda, S. Furuya, R. Fukai, A. Fujii, Y. Cho, M. Arakawa, M. Abe, Y. Tsuda
Publikováno v:
Science
Science, 2022, 379 (6634), ⟨10.1126/science.abn8671⟩
Science, 379(6634)
Science, 2022, 379 (6634), ⟨10.1126/science.abn8671⟩
Science, 379(6634)
Samples of the carbonaceous asteroid Ryugu were brought to Earth by the Hayabusa2 spacecraft. We analyzed 17 Ryugu samples measuring 1 to 8 millimeters. Carbon dioxide–bearing water inclusions are present within a pyrrhotite crystal, indicating tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::37fcce288dc15c177dd05920e68006c7
https://hal.science/hal-03854309/document
https://hal.science/hal-03854309/document
Autor:
S. M. Hall, J. S. Beard, C. J. Potter, R. J. Bodnar, L. A. Neymark, J. B. Paces, C. A. Johnson, G. N. Breit, R. A. Zielinski, G. J. Aylor
The Coles Hill uranium deposit, with an indicated resource of about 130 Mlb of U3O8, is the largest unmined uranium deposit in the United States. The deposit is hosted in the Taconian (approx. 480-450 Ma) Martinsville igneous complex, which consists
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::58e35f5cc6cd9a68fbbb129a2d26a3e1
https://hdl.handle.net/10919/109781
https://hdl.handle.net/10919/109781
Autor:
Guoji Wang, Linda M. Dallasta, Cristian L. Achim, Clayton A. Wiley, R Draviam, R J Bodnar, Ronald L. Hamilton
Publikováno v:
Neuropathology and Applied Neurobiology. 26:332-341
The cell adhesion molecules, intercellular adhesion molecule (ICAM)-1 and vascular cell adhesion molecule (VCAM)-1, are important mediators of immune interactions within the central nervous system (CNS). A wide variety of pro-inflammatory insults to
Autor:
R. J. Bodnar, William O. Roberts
Publikováno v:
The Physician and Sportsmedicine. 26:16-19
(1998). Technique for Face Mask Removal. The Physician and Sportsmedicine: Vol. 26, No. 12, pp. 16-19.
Publikováno v:
Geobiology. 10(5)
The identification and confirmation of bona fide Archean-Paleoproterozoic microfossils can prove to be a challenging task, further compounded by diagenetic and metamorphic histories. While structures of likely biological origin are not uncommon in Pr
Publikováno v:
Mineralogical Magazine-Goldschmidt Conference Abstracts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0135fb1cade63d75eb99b540a7bd85ba
https://gfzpublic.gfz-potsdam.de/pubman/item/item_243922
https://gfzpublic.gfz-potsdam.de/pubman/item/item_243922
Autor:
John K. Costain, R. J. Bodnar
Publikováno v:
Geophysical Research Letters. 18:983-986
The ability of fluids flowing through a given volume of crustal rock to affect mass and energy transfer is controlled by the physical and chemical nature of the fluid. Most numerical simulations of fluid-flow and fluid-rock interaction approximate th