Clay orientation in some Upper Carboniferous mudrocks, its relationship to quartz content and some inferences about fissility, porosity and compactional history
- 14 June 1980
- journal article
- Published by Wiley in Sedimentology
- Vol. 27 (3), 333-339
- https://doi.org/10.1111/j.1365-3091.1980.tb01183.x
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Geochemistry of the Hepworth Carboniferous sediment sequence and origin of the diagenetic iron minerals and concretionsGeochimica et Cosmochimica Acta, 1979
- Size distribution of quartz in mudrocksSedimentology, 1976
- The fissility of some Carboniferous shalesSedimentology, 1976
- Shale fissility: relation to bioturbationSedimentology, 1974
- Clay-Ironstone Concretion Preserving Fabrics Due to Progressive CompactionGSA Bulletin, 1972
- MICRO‐FABRICS OF SHALES AND THEIR REARRANGEMENT BY COMPACTIONSedimentology, 1970
- THE FABRIC OF SHALE—AN ELECTRON‐MICROSCOPE STUDYSedimentology, 1970
- X-Ray Analysis of Preferred Orientation in Fine-Grained Quartz AggregatesThe Journal of Geology, 1969
- The Determination of Quartz in Sedimentary Rocks Using an X-Ray Diffraction MethodClays and Clay Minerals, 1969
- Chapter 4 Diagenesis in Argillaceous SedimentsPublished by Elsevier ,1967