Early Cambrian transgression
- 1 March 1979
- journal article
- Published by Geological Society of London in Journal of the Geological Society
- Vol. 136 (2) , 133-135
- https://doi.org/10.1144/gsjgs.136.2.0133
Abstract
There is widespread evidence of a major transgression near the base of the Cambrian. It is difficult to establish time-controls, and therefore difficult to produce worthwhile estimates of rate of transgression. Neither the palaeontological nor the radiometric information is sufficiently exact. Alternative means of comparing the Cambrian transgression with later events of the same kind are sought; the possibility that it is due to post-glacial (i.e. post-Varangian) rise of sea level is examined and rejected; the separation in time seems too large. The preferred explanation is that the Cambrian transgression had tectonic causes and it is argued that among the major transgressions of later geological time, it is the Cretaceous case which most closely resembles the Cambrian.This publication has 11 references indexed in Scilit:
- I.U.G.S./I.G.C.P. Project 29 Precambrian–Cambrian Boundary Working Group in Cambridge, 1978Geological Magazine, 1978
- On the Late Precambrian–Early Cambrian Hartshill Formation of WarwickshireGeological Magazine, 1978
- The Cambrian SystemPublished by American Association of Petroleum Geologists AAPG/Datapages ,1978
- The Mesozoic development of aseismic continental marginsJournal of the Geological Society, 1977
- Fossil data and the Precambrian-Cambrian evolutionary transitionAmerican Journal of Science, 1976
- Small shelly fossils of late Precambrian and early Cambrian age: a review of recent workJournal of the Geological Society, 1975
- RELATIONSHIPS OF CRATONIC AND CONTINENTAL-MARGIN TECTONIC EPISODESPublished by Society for Sedimentary Geology ,1974
- THE LOWER CAMBRIAN FOSSIL TOMMOTIALethaia, 1970
- The Great Infra-Cambrian Ice AgeScientific American, 1964
- Sequences in the Cratonic Interior of North AmericaGSA Bulletin, 1963