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- W4315694687 abstract "In this chapter we discuss the role of groundwater and other fluids in metamorphism. Metamorphism is a broad term that encompasses all adjustments of solid rocks to changes in physical and chemical conditions. It thus includes diagenesis, a more narrowly defined term that is specific to changes undergone by sediments after initial deposition and during and after lithification. We consider diagenesis elsewhere: compaction and associated diagenesis in sedimentary basins is treated in Chapter 11 and the diagenesis of carbonate platforms in Section 13.8. Further, diagenetic processes within accretionary prisms are mentioned in Section 13.7. In this book, then, we use diagenesis to refer to chemical, physical, and biological changes undergone by sediments in a typical sedimentary environment (P generally <100 MPa, T generally <100 ◦C). Though there is no hard and fast distinction between diagenesis and metamorphism, we have reserved the term metamorphism to refer to changes in the solid state at greater pressures and/or temperatures. There is a further distinction between contact metamorphism, which takes place near an igneous intrusion, and the regional metamorphism that occurs in orogenic belts at a wide range of pressures and temperatures. In both types of metamorphism there is generally a gain, loss, and/or exchange of chemical constituents via a fluid phase, a process sometimes termed metasomatism." @default.
- W4315694687 created "2023-01-12" @default.
- W4315694687 date "2006-05-04" @default.
- W4315694687 modified "2023-09-27" @default.
- W4315694687 title "Metamorphism" @default.
- W4315694687 doi "https://doi.org/10.1017/9780511807855.013" @default.
- W4315694687 hasPublicationYear "2006" @default.
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