Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Australasian tektite"'
Autor:
Toshihiro Tada, Ryuji Tada, Praphas Chansom, Wickanet Songtham, Paul A. Carling, Eiichi Tajika
Publikováno v:
Progress in Earth and Planetary Science, Vol 7, Iss 1, Pp 1-15 (2020)
Abstract There are several reports of Australasian tektites found within a stratum called “laterite” layer widely distributed in Indochina. However, it has been debated whether these tektites are in situ or reworked. This uncertainty is because a
Externí odkaz:
https://doaj.org/article/f5475e032b824a17b9d3bb24e5f48755
Supporting data for manuscript:TiO2II: the high-pressure Zr-free srilankite endmember in impact rocks.Included here: Raman spectroscopy data, PACOM map, all HRTEM data, and 3DED raw data of cr04 (TiO2II sample 1144a_16), cr09 (coesitesample 1144a_12)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::248776510cb7e38a330881ca4e3cf85e
Akademický článek
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Publikováno v:
Meteoritics & Planetary Science. 55:253-273
We examined 16 white opaque inclusions exposed on two polished slices of a Muong Nong-type Australasian tektite from Muong Phin, Laos. The inclusions usually consist of a core, surrounded by a froth layer, and a quartz neoblast layer. The cores are c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b78bc55f6930cdbae52ea6dda8572dea
https://doi.org/10.1111/maps.13433
https://doi.org/10.1111/maps.13433
Autor:
Whymark, Aubrey
Thai Geoscience Journal, 2, 2, 1 ถึง 30
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::494f1a7105161ccef26f1cb5381a7f70
Publikováno v:
Geochimica et cosmochimica acta 298 (2021): 112–130. doi:10.1016/j.gca.2021.01.046
info:cnr-pdr/source/autori:Di Vincenzo G.[1], Folco L.[2,3], Suttle M.D.[2,4], Brase L.[5], Harvey R.P.[5]/titolo:Multi-collector 40Ar%2F39Ar dating of microtektites from Transantarctic Mountains (Antarctica): A definitive link with the Australasian tektite%2Fmicrotektite strewn field/doi:10.1016%2Fj.gca.2021.01.046/rivista:Geochimica et cosmochimica acta/anno:2021/pagina_da:112/pagina_a:130/intervallo_pagine:112–130/volume:298
info:cnr-pdr/source/autori:Di Vincenzo G.[1], Folco L.[2,3], Suttle M.D.[2,4], Brase L.[5], Harvey R.P.[5]/titolo:Multi-collector 40Ar%2F39Ar dating of microtektites from Transantarctic Mountains (Antarctica): A definitive link with the Australasian tektite%2Fmicrotektite strewn field/doi:10.1016%2Fj.gca.2021.01.046/rivista:Geochimica et cosmochimica acta/anno:2021/pagina_da:112/pagina_a:130/intervallo_pagine:112–130/volume:298
Microtektites represent high-velocity/distal meteorite impact ejecta. Demonstrating that microtektites found at several locations throughout East-Antarctica consist of a homogeneous class of geological objects belonging to the Australasian tektite/mi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5fbc5e453521ce7cd54f6eee769b6fe5
Publikováno v:
Geochimica et Cosmochimica Acta. 217:28-50
The Australasian tektite strewn field is exceptional, not only as the largest and most recent, but also as the only strewn field without an identified source impact crater. Therefore, scenarios without the formation of an impact crater, such as a low
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f2b056b6ba0167e3be454a3611481ef9
https://doi.org/10.1016/j.gca.2017.08.013
https://doi.org/10.1016/j.gca.2017.08.013
Autor:
Mauro Gemmi, Luke Daly, Luigi Folco, Billy P. Glass, Martin Lee, Enrico Mugnaioli, F. Campanale
Coesite, a high-pressure silica polymorph, is a diagnostic indicator of impact cratering in quartz-bearing target rocks. The formation mechanism of coesite during hypervelocity impacts has been debated since its discovery in impact rocks in the 1960s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7ee643aa14d25df2337a34142e61d944
http://hdl.handle.net/11365/1117912
http://hdl.handle.net/11365/1117912
Akademický článek
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Akademický článek
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