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Number of results
2014 | 5 | 21-24

Article title

Topliwość tektytów

Content

Title variants

EN
Tektites melting

Languages of publication

PL

Abstracts

EN
In this paper, results of melting experiment of tektites are presented. Tektites from four strewnfields: North American, Central European, Ivory Coast and Australasian were used. The fragments of investigated tektites were heated in oxide atmosphere in 1100oC in two time intervals: 5 and 120 minutes. The temperature of 1100oC is too low for completely melting of the studied material despite to heating in the same conditions but in small area (eg. in a spot).

Keywords

Year

Volume

5

Pages

21-24

Physical description

Contributors

  • Uniwersytet– Śląski, Wydział Nauk o Ziemi, Katedra Geochemii, Mineralogii i Petrografii
  • Uniwersytet– Śląski, Wydział Nauk o Ziemi, Katedra Geochemii, Mineralogii i Petrografii
  • Pracownia Badań Rentgenostrukturalnych, Wydział Nauk o Ziemi UŚ
  • Uniwersytet– Śląski, Wydział Nauk o Ziemi, Katedra Geochemii, Mineralogii i Petrografii

References

  • French B.M., 1998, Traces of Catastrophe. A Handbook of Shock-Metamorphic Effects in Terrestrial Meteorite Impact Structures, Lunar and Planetary Institute, Boulevard.
  • Glass B.P., Simonson B.M., 2013, Distal impact ejecta layers. A record of large impacts in sedimentary deposits, Impact Studies, Springer, Berlin–Heidelberg.
  • Glass B.P., Muenow D.W., Bohor B.F., Meeker G.P., 1997, Fragmentation and hydration of tektites and microtektites, Meteoritics & Planetary Science, 32, s. 333–341.
  • Koeberl C., Poag C.W., Reimold W.U., Brandt D., 1996, Impact origin of the Chesapeake Bay structure and the source of the North American tektites, Science, 271, s. 1263–1266.
  • Poag C.W., Powars D.S., Poppe L.J., Mixon R.B., 1994, Meteoroid mayhem in Ole Virginny: Source of the North American tektite strewn field, Geology, 22, s. 691–694.

Document Type

article

Publication order reference

Identifiers

YADDA identifier

bwmeta1.element.psjd-36685db2-ef08-47c4-b605-ce9808f6a340
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