作者: P. W. Lipman , S. Aramaki
DOI: 10.1086/627196
关键词: Petrology 、 Geotechnical engineering 、 Flow (psychology) 、 Compaction 、 Geology
摘要: Near Takachiho Town, Kyushu, Japan, four welded-tuff units, which are interbedded with tuffaceous sediments and closely resemble a sequence of thin, separate ash-flow sheets, actually consist disrupted parts single originally continuous sheet. Separations between the welded units represent pull-apart structures resulting from tensional fracturing cooling upper sheet simultaneous further compaction possible flowage hotter interior over buried irregular preemption surface. After intervening voids were filled by water-transported sediments.