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The /Tertiary boundary interval, Raton Basin, and , and its content of shock-metamorphosed minerals; Evidence relevant to the KIT boundary impact-extinction theory Glen A. Izett

CLEAR CREEK NORTH SITE, COLO

ICoa/

Impact Layer,

C/aysfoneB|

Carbonaceous HS/ia/eK

SPECIAL PAPER 249

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The Cretaceous/Tertiary boundary interval, Raton Basin, Colorado and New Mexico, and its content of shock-metamorphosed minerals; Evidence relevant to the K/T boundary impact-extinction theory

Glen A. Izett U.S. Geological Survey M.S. 913, Box 25046 Denver Federal Center Denver, Colorado 80225

5FEC1IIPAPEH 249

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Published by The Geological Society of America, Inc. 3300 Penrose Place, P.O. Box 9140, Boulder, Colorado 80301

GSA Books Science Editor Richard A. Hoppin

Printed in U.S.A.

Library of Congress Cataloging-in-Publication Data Izett, Glen Arthur, 1928- The Cretaceous/Tertiary boundary interval, Raton Basin, Colorado and New Mexico, and its content of shock-metamorphosed minerals : evidence relevant to the K/T boundary impact-extinction theory / Glen A. Izett. p. cm.—(Special paper / Geological Society of America ; 249) Includes bibliographical references. ISBN 0-8137-2249-7 1. Cretaceous/Tertiary boundary—Raton Basin (Colo, and N.M.) 2. —Raton Basin (Colo, and N.M.) 3. Mineralogy—Raton Basin (Colo, and N.M.) I. Title. II. Series: Special papers (Geological Society of America); 249. QE689.I94 1990 551,7'7'0978896—dc20 90-3737 CIP

Cover photos: Front, K/T interval from the Clear Creek North site, Colorado (Continental rocks in western United States). Back, K/T interval from the Stevns Klint, Denmark, site (Marine rocks in Europe).

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