Transcription of Porosity and Bulk Density of Sedimentary Rocks
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Porosity and Bulk Density of Sedimentary Rocks
Porosity and Bulk Density of Sedimentary Rocks ~y G. EDWARD MANGER :ONTRIBUTIONS TO GEOCHEMISTRY GEOLOGICAL SURVEY BULLETIN 1144-E Prepared partly on behalf of the Atomic Energy Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEW ART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, Government Printing Office Washington, , 20402 CONTENTS Page Abstract-------------------------------- --------------------------E1 Introduction_____ 1 Methods of Porosity determination _____ ------_____ -------_ 45 lteferences----------------------------- ---------------------------47 TABLES TABLE 1. Sandstone, siltstone, quartzite, chert, and conglomerate_____ E5 2. Limestone, dolomite, chalk, and marble_____ 26 3. Shale, claystone, and slate_____ 36 4. Unconsolidated materials_____ 41 5. Other rock types_____ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 44 m CONTRIBUTIONS TO GEOCHEMISTRY Porosity AND BULK Density OF Sedimentary Rocks By G.
porosity, the average dry and saturated bulk density, the source of the data, and the method of porosity determination. The tabulation reflects the fact that more porosity than density data for sedimentary rocks are available in the literature. The stratigraphic nomenclature in this report is from various sources and does not necessarily follow
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