2 edition of system K₂O-MgO-SiO₂ found in the catalog.
system K₂O-MgO-SiO₂
Edwin Woods Roedder
Published
1951
by Carnegie Institution of Washington in Washington
.
Written in
Edition Notes
Statement | Edwin Woods Roedder. |
Series | Papers from the Geophysical Laboratory, Carnegie Institution of Washington ;, no. 1140 |
Classifications | |
---|---|
LC Classifications | QE389.62 .R6 |
The Physical Object | |
Pagination | 81-180, 224-248 p. ; |
Number of Pages | 248 |
ID Numbers | |
Open Library | OL6091867M |
LC Control Number | 51008751 |
OCLC/WorldCa | 14009201 |
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A collapsing gully system consists of five parts (Xu, ; Xia et al., ): upper catchment, collapsing wall, colluvial deposit, scour channel and alluvial fan (), while slumps and massive collapses of the collapsing wall are one of the main influential factors for the collapsing gully enlargement and development (Xia et al., ).According to classical soil mechanics, the stability of the Cited by: 3.
A collapsing gully system consists of five parts (Xu, ; Xia et al., ): upper catchment, collapsing wall, colluvial deposit, scour channel and alluvial fan (), while slumps and massive collapses of the collapsing wall are one of the main influential factors for the collapsing gully enlargement and development (Xia et al., ).According to classical soil mechanics, the stability of the.
A collapsing gully system consists of five parts (Xu, ; Xia et al., ): upper catchment, collapsing wall, colluvial deposit, scour channel and alluvial fan (), while slumps and massive collapses of the collapsing wall are one of the main influential factors for the collapsing gully enlargement and development (Xia et al., ).According to classical soil mechanics, the stability of the.