Distal Impact Ejecta Layers

A Record of Large Impacts in Sedimentary Deposits

  • Billy P. Glass
  • Bruce M. Simonson

Part of the Impact Studies book series (IMPACTSTUD)

Table of contents

  1. Front Matter
    Pages i-xv
  2. Billy P. Glass, Bruce M. Simonson
    Pages 1-13
  3. Billy P. Glass, Bruce M. Simonson
    Pages 137-243
  4. Billy P. Glass, Bruce M. Simonson
    Pages 245-320
  5. Billy P. Glass, Bruce M. Simonson
    Pages 321-369
  6. Billy P. Glass, Bruce M. Simonson
    Pages 371-418
  7. Billy P. Glass, Bruce M. Simonson
    Pages 419-497
  8. BillyP Glass, BruceM Simonson
    Pages 499-532
  9. Billy P. Glass, Bruce M. Simonson
    Pages 595-624
  10. Back Matter
    Pages 625-716

About this book

Introduction

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

Keywords

Distal Impact Ejecta Impact Spherules Microkrystites Microtektites Shock Metamorphism

Authors and affiliations

  • Billy P. Glass
    • 1
  • Bruce M. Simonson
    • 2
  1. 1.Dept. GeologyUniversity of DelawareNewarkUSA
  2. 2.Dept. GeologyOberlin CollegeOberlinUSA

Bibliographic information

  • DOI https://doi.org/10.1007/978-3-540-88262-6
  • Copyright Information Springer-Verlag Berlin Heidelberg 2013
  • Publisher Name Springer, Berlin, Heidelberg
  • eBook Packages Earth and Environmental Science
  • Print ISBN 978-3-540-88261-9
  • Online ISBN 978-3-540-88262-6
  • Series Print ISSN 1612-8338
  • About this book