4 edition of The tertiary welded-tuff vent agglomerate and associated rocks at Sandy Braes, Co. Antrim found in the catalog.
The tertiary welded-tuff vent agglomerate and associated rocks at Sandy Braes, Co. Antrim
I. B. Cameron
Bibliography: p. 14-15.
|Statement||by I. B. Cameron & P. A. Sabine.|
|Series||Institute of Geological Sciences. Report no. 69/6, Report (Institute of Geological Sciences (Great Britain)) ;, 69/6.|
|Contributions||Sabine, Peter Aubrey, joint author.|
|LC Classifications||QE461 .C35|
|The Physical Object|
|Pagination||iv, 15 p.|
|Number of Pages||15|
|LC Control Number||73574598|
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Get this from a library. The tertiary welded-tuff vent agglomerate and associated rocks at Sandy Braes, Co. Antrim. [I B Cameron; Peter Aubrey Sabine]. Abstract. Our knowledge of the sea bottom of the North Polar Sea, the Greenland-Norwegian Sea, and the North Atlantic was for a long period based on bathymetric maps by Nansen () and bottom-sample investigations by Bøggild (, ).Cited by: The modification of various kinds of sedimentary rocks upon burial has largely been studied by investigators from different sub-disciplines within the earth sciences: (1) changes in mineralogy of clay-rich sedimentary rocks by sedimentary petrographers and clay mineralogists; (2) authigenic mineral assemblages in tuffs and volcanic sediments by Cited by: developments in sedimentology 25b diagenesis in sediments and sedimentary rocks, 2 further titles in this series volumes 1, 2, 3, 5, 8 and 9 are out of print 4 f.g.
t i c k e l l the techniques of sedimentary mineralogy 6 l. v a n d e r p l a s the identification o f detrital feldspars i s. d z u l y n s k i and e.k. w a l t o n sedimentary features o f flysch and greywackes d. duff, a.