Abstract
We give spatial patterns of distribution of the principal groups of lithologic associations (sedimentary and volcanogenicl and a quantitative estimate of their volumes and distribution for each of the three series of the Cambrian system on the present continents. In conclusion, we make some suggestions as to changes in tectonic regime, features of sedimentation, and paleogeographic conditions during the Cambrian period.—Authors.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
