Scientific Library of Tomsk State University

   E-catalog        

Image from Google Jackets
Normal view MARC view

Distal Impact Ejecta Layers [electronic resource] : A Record of Large Impacts in Sedimentary Deposits / by Billy P. Glass, Bruce M. Simonson.

By: Glass, Billy P [author.]Contributor(s): Simonson, Bruce M [author.] | SpringerLink (Online service)Material type: TextTextSeries: Impact StudiesPublication details: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2013Description: XV, 716 p. 280 illus., 16 illus. in color. online resourceContent type: text Media type: computer Carrier type: online resourceISBN: 9783540882626Subject(s): geography | geology | Physical geography | Sedimentology | Planetology | earth sciences | Geology | Geophysics/Geodesy | Planetology | SedimentologyDDC classification: 551 LOC classification: QE1-996.5Online resources: Click here to access online
Contents:
Impact Crater Formation -- Distal Impact Ejecta Layers -- Modeling Variations in Distal Impact -- Distal Impact Ejecta Layers and Earth History.
In: Springer eBooksSummary: Impact cratering is an important geological process on all solid planetary bodies, and, in the case of Earth, may have had major climatic and biological effects. Most terrestrial impact craters have been erased or modified beyond recognition. However, major impacts throw ejecta over large areas of the Earth's surface. Recognition of these impact ejecta layers can help fill in the gaps in the terrestrial cratering record and at the same time provide direct correlation between major impacts and other geological events, such as climatic changes and mass extinctions. This book provides the first summary of known distal impact ejecta layers
Tags from this library: No tags from this library for this title. Log in to add tags.
No physical items for this record

Impact Crater Formation -- Distal Impact Ejecta Layers -- Modeling Variations in Distal Impact -- Distal Impact Ejecta Layers and Earth History.

Impact cratering is an important geological process on all solid planetary bodies, and, in the case of Earth, may have had major climatic and biological effects. Most terrestrial impact craters have been erased or modified beyond recognition. However, major impacts throw ejecta over large areas of the Earth's surface. Recognition of these impact ejecta layers can help fill in the gaps in the terrestrial cratering record and at the same time provide direct correlation between major impacts and other geological events, such as climatic changes and mass extinctions. This book provides the first summary of known distal impact ejecta layers

There are no comments on this title.

to post a comment.