FIAMME FORMED BY DIAGENESIS AND BURIAL-COMPACTION IN SOILS AND SUBAQUEOUS SEDIMENTS

被引：44

作者：

BRANNEY, MJ ^{[1
]}

SPARKS, RSJ ^{[1
]}

机构：

[1] UNIV BRISTOL,DEPT GEOL,BRISTOL BS8 1RJ,ENGLAND

来源：

JOURNAL OF THE GEOLOGICAL SOCIETY | 1990年 / 147卷

关键词：

D O I：

10.1144/gsjgs.147.6.0919

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Pumice clasts can be diagenetically altered at low temperature and flattened by compaction to form fiamme. Examples are described from trachytic pumice fall layers alternating with palaeosoils on Sao Miguel in the Azores and from Ordovician lacustrine volcaniclastic sedimentary rocks from the English Lake District.

引用

页码：919 / 922

页数：4

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