Zobrazeno 1 - 10
of 60
pro vyhledávání: '"Jouko Raitala"'
Autor:
Ramon Egli, Myriam Kars, N. S. Bezaeva, Pierre Rochette, Jouko Raitala, Joshua M. Feinberg, Jérôme Gattacceca, Dmitrii D. Badyukov, D. M. Kuzina
Publikováno v:
Meteoritics and Planetary Science
Meteoritics and Planetary Science, Wiley, 2018, 53 (1), pp.131-150. ⟨10.1111/maps.13006⟩
Meteoritics and Planetary Science, 2018, 53 (1), pp.131-150. ⟨10.1111/maps.13006⟩
Meteoritics and Planetary Science, Wiley, 2018, 53 (1), pp.131-150. ⟨10.1111/maps.13006⟩
Meteoritics and Planetary Science, 2018, 53 (1), pp.131-150. ⟨10.1111/maps.13006⟩
Hypervelocity impacts occur on bodies throughout our solar system, and play an important role in altering the mineralogy, texture, and magnetic properties in target rocks at nanometer to planetary scales. Here we present the results of hypervelocity
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a5262760babc7ba8dcbf260912dc79e4
https://doi.org/10.1111/maps.13006
https://doi.org/10.1111/maps.13006
Publikováno v:
Planetary and Space Science. 140:35-48
The large scale outflow channels of the Hellas impact basin are characteristic to its eastern rim region. Although the majority of the valles are located in the large-scale topographic trough connecting Hesperia Planum and Hellas basin, the most far-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::014156ab14a92d29f625bb9d934ce774
https://doi.org/10.1016/j.pss.2017.04.001
https://doi.org/10.1016/j.pss.2017.04.001
Publikováno v:
Petrology. 23:103-115
The Chelyabinsk meteorite (which fell on February 15, 2013) is a LL5 chondrite of shock stage S4, whose fragments are classified into light and dark lithologies. According to the intensity of their shock metamorphism, light lithology fragments are su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1004fce8be4df9f866441878f8319c2
https://doi.org/10.1134/s0869591115020022
https://doi.org/10.1134/s0869591115020022
Autor:
Mikhail A. Ivanov, Jouko Raitala, T. Törmänen, E. N. Guseva, V. P. Kostama, A. M. Abdrakhimov, J. Korteniemi
Publikováno v:
Solar System Research. 48:130-138
This paper presents morphometric parameters of Martian layered sequences of different origin that outcrop in the scarps and crater walls, which form natural geologic profiles. The objective of this study was to develop quantitative criteria that woul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ae0ed1f66167649b33af33727fa7ce7
https://doi.org/10.1134/s003809461402004x
https://doi.org/10.1134/s003809461402004x
Publikováno v:
Planetary and Space Science. 59:1195-1209
The study is a detailed look on one of the several fluvial systems located on the eastern rim region of the Hellas basin on Mars. We analyzed the morphologic and morphometric characteristics of an extensive channel system, which extends for over 650
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b63ff38af853f9b415032f2fb553b6c
https://doi.org/10.1016/j.pss.2010.09.009
https://doi.org/10.1016/j.pss.2010.09.009
Publikováno v:
Geochemistry International. 49:641-653
Soil layers at the Tunguska event site may have accumulated infalling extraterrestrial matter derived from the Tunguska Cosmic Body (TCB). Using mineralogical, textural, and chemical criteria, a set of metal and silicate spherules of probably cosmic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::984372b3487bcf8d9d9e31ce2efacbc3
https://doi.org/10.1134/s0016702911070032
https://doi.org/10.1134/s0016702911070032
Publikováno v:
Meteoritics & Planetary Science. 45:1502-1512
– A large number of micrometeorites (MMs) was recovered from glacier deposits located at the north-eastern passive margin of the Novaya Zemlya glacier sheet. Melted, scoriaceous, and unmelted micrometeorites (UMMs) are present. Unmelted micrometeor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5383138c9f870cc49f55b124837d9a4
https://doi.org/10.1111/j.1945-5100.2010.01125.x
https://doi.org/10.1111/j.1945-5100.2010.01125.x
Autor:
Jouko Raitala, David A. Williams, Harold Clenet, Patrick Pinet, C. Rosemberg, Ronald Greeley, Thomas B. McCord, L. Manfredi, Francois Poulet, J. P. Combe, Robin L. Fergason, Gerhard Neukum
Publikováno v:
Earth and Planetary Science Letters. 294:451-465
We used Thermal Emission Spectrometer (TES), Thermal Emission Imaging System (THEMIS), High-Resolution Stereo Camera (HRSC), and Observatoire pour la Mineralogie, l'Eau, les Glaces et l'Activite (OMEGA) data to assess the physical and compositional p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e08dc3736fbbc4caffba22c220cee1be
https://doi.org/10.1016/j.epsl.2009.11.019
https://doi.org/10.1016/j.epsl.2009.11.019
Publikováno v:
Earth and Planetary Science Letters. 294:321-331
Four prominent fluvial systems, Dao, Niger, and Harmakhis Valles, and a system of smaller channels between Niger and Harmakhis Valles characterize a wide topographic trough that connects Hesperia Planum and Hellas Planitia (Hesperia–Hellas trough,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01b11a70013418d701390ff0e4d9d41e
https://doi.org/10.1016/j.epsl.2009.11.021
https://doi.org/10.1016/j.epsl.2009.11.021
Autor:
J. Korteniemi, V. P. Kostama, Teemu Öhman, Mikhail A. Ivanov, M. Aittola, Jouko Raitala, Harald Hiesinger
Publikováno v:
Earth and Planetary Science Letters. 294:466-478
The eastern Hellas basin rim has been highly modified by a multitude of both volcanic and fluvial processes. It is covered by a large part of the Circum-Hellas Volcanic Province, consisting of the volcanic plains of Hesperia Planum and western Promet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ca5126360939717747c5e2d70204852
https://doi.org/10.1016/j.epsl.2009.06.038
https://doi.org/10.1016/j.epsl.2009.06.038