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Ch. 1 | An Introduction to Clay Minerals and Isotope Geochemistry | 1 |
Ch. 2 | Isotope Geochemistry of Clay Minerals in Continental Weathering Environments | 60 |
Ch. 3 | Isotope Geochemistry of Clay Minerals in Young Continental and Oceanic Sediments | 105 |
Ch. 4 | Isotope Geochemistry of Clays and Clay Minerals from Sedimentary Rocks | 180 |
Ch. 5 | Isotope Geochemistry of Mica-Type Minerals from Low-Temperature Metamorphic Rocks | 263 |
Ch. 6 | The Frontiers of Clay Isotope Geochemistry | 304 |
References | 325 | |
Subject Index | 355 |
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Add Clays in Crustal Environments: Isotope Dating and Tracing, Clay minerals form in a wide variety of crustal environments, e.g. in soil profiles, in sediments at the surface and in deeply buried sedimentary deposits, and under regional, contact and hydrothermal metamorphism conditions. The book provides informa, Clays in Crustal Environments: Isotope Dating and Tracing to the inventory that you are selling on WonderClubX
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Add Clays in Crustal Environments: Isotope Dating and Tracing, Clay minerals form in a wide variety of crustal environments, e.g. in soil profiles, in sediments at the surface and in deeply buried sedimentary deposits, and under regional, contact and hydrothermal metamorphism conditions. The book provides informa, Clays in Crustal Environments: Isotope Dating and Tracing to your collection on WonderClub |