Abstract
Identifies two kinds of breccia; type A limestone breccia (LBA) and type B limestone breccia (LBB). These rocks are characterized by polymictic components, wide-ranging sizes, poor sorting, dense packing and disorganized fabrics of shallow-marine limestone clasts and generally small proportions of a matrix. Decrease in clast-size and increase of abraded clasts from the LBB to the limestone sandstone imply a depositional progression from the LBB through the limestone debris-crowded rock and limestone conglomerate to the limestone sandstone. -from Authors
Original language | English |
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Pages (from-to) | 297-309 |
Number of pages | 13 |
Journal | Journal - Geological Society of Japan |
Volume | 97 |
Issue number | 4 |
Publication status | Published - Jan 1 1991 |
All Science Journal Classification (ASJC) codes
- Environmental Science(all)
- Engineering(all)
- Earth and Planetary Sciences(all)