Abstract:An attempt is made at explaining the successive origin of the central peaks and terrace ring-wall in the crater formations filled with melt after impacts.
“…The volume of a solid crystallized basalt is 3-10% smaller than the volume of the original melt. In the solidifying volumes of spherical shapes large cavities are formed in the centre (Kopecky, 1971).…”
mentioning
confidence: 99%
“…Possible relations between meteorite impact and igneous petrogenesis were discussed also by French (1970).…”
An attempt is made at explaining the successive origin of the central peaks and terrace ring-wall in the crater formations filled with melt after impacts.
“…The volume of a solid crystallized basalt is 3-10% smaller than the volume of the original melt. In the solidifying volumes of spherical shapes large cavities are formed in the centre (Kopecky, 1971).…”
mentioning
confidence: 99%
“…Possible relations between meteorite impact and igneous petrogenesis were discussed also by French (1970).…”
An attempt is made at explaining the successive origin of the central peaks and terrace ring-wall in the crater formations filled with melt after impacts.
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