Lithofacies, Depositional Environments, and Regional Stratigraphy of the Lower Eocene Ghazij Formation, Balochistan, Pakistan
U.S. Department of the Interior U.S. Geological Survey Lithofacies, Depositional Environments, and Regional Stratigraphy of the Lower Eocene Ghazij Formation, Balochistan, Pakistan U.S. Geological Survey Professional Paper 1599 Prepared in cooperation with the Geological Survey of Pakistan A Cover. Exposures of the lower Eocene Ghazij Formation along the northeast flank of the Sor Range, Balochistan, Pakistan. Photograph by Stephen B. Roberts. Lithofacies, Depositional Environments, and Regional Stratigraphy of the Lower Eocene Ghazij Formation, Balochistan, Pakistan By Edward A. Johnson, Peter D. Warwick, Stephen B. Roberts, and Intizar H. Khan U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1599 Prepared in cooperation with the Geological Survey of Pakistan UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1999 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Lithofacies, depositional environments, and regional stratigraphy of the lower Eocene Ghazij Formation, Balochistan, Pakistan / by Edward A. Johnson . .[et al.]. p. cm.—(U.S. Geological Survey professional paper ; 1599) "Prepared in cooperation with the Geological Survey of Pakistan." Includes bibliographical references. 1. Geology, Stratigraphic—Eocene. 2. Geology—Pakistan— Balochistan. 3. Coal—Geology—Pakistan—Balochistan. 4. Ghazij Formation (Pakistan). I. Johnson, Edward A. (Edward Allison), 1940- . II. Series. QE692.2.L58 1999 553.2'4'0954915—dc21 98-3305 ISBN=0-607-89365-6 CIP CONTENTS Abstract..........................................................................................................................
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