The Stratigraphy and Paleontology of the Nipissing and Mattawa Areas
Author : D. J. Colquhoun
Publisher :
Page : pages
File Size : 39,65 MB
Release : 1956
Category :
ISBN :
Author : D. J. Colquhoun
Publisher :
Page : pages
File Size : 39,65 MB
Release : 1956
Category :
ISBN :
Author :
Publisher :
Page : 1030 pages
File Size : 41,79 MB
Release : 1965
Category : Geology
ISBN :
Author : Bailey Willis
Publisher :
Page : 918 pages
File Size : 12,85 MB
Release : 1912
Category : Geology
ISBN :
Author : Ontario. Department of Mines
Publisher :
Page : 42 pages
File Size : 47,7 MB
Release : 1960
Category : Dissertations, Academic
ISBN :
Author : Madeleine Alberta Fritz
Publisher :
Page : 137 pages
File Size : 15,93 MB
Release : 1925
Category : Echinodermata
ISBN :
Author :
Publisher :
Page : 1032 pages
File Size : 16,42 MB
Release : 1965
Category : Geology
ISBN :
1919/28 cumulation includes material previously issued in the 1919/20-1935/36 issues and also material not published separately for 1927/28. 1929/39 cumulation includes material previously issued in the 1929/30-1935/36 issues and also material for 1937-39 not published separately.
Author : Geological Survey (U.S.)
Publisher :
Page : 916 pages
File Size : 11,69 MB
Release : 1912
Category : Geology
ISBN :
Author : Geological Survey (U.S.)
Publisher :
Page : 1028 pages
File Size : 47,66 MB
Release : 1965
Category :
ISBN :
Author : Matthew H. Nitecki
Publisher : Springer Science & Business Media
Page : 249 pages
File Size : 42,3 MB
Release : 2012-12-06
Category : Science
ISBN : 1461546915
Receptaculitids are extinct high-level fossils that provide a window into the history of life. After the discovery and analysis of a deposit of phosphatized receptaculitids on the Baltic Sea island of Öland, the authors conclude that receptaculitids possess an attribute not found in any other group of organisms, living or fossil.
Author : Donald J. Colquhoun
Publisher :
Page : 352 pages
File Size : 15,48 MB
Release : 1960
Category : Alberta
ISBN :
The area to be considered lies east from the Rocky Mountain Front to the eastern erosion edge of the Triassic strata in the subsurface. It therefore includes both surface and subsurface sections. All Triassic strata lying between latitude 53° and 59° 30' (and consequently between the Whitehorse Creek and Liard River type sections) are considered.