The Tourmaline Group in Sediments
Paul D. Krynine
Abstract
Paul D. Krynine
Abstract
Tourmaline is really a complex isomorphous mineral group which can be easily differentiated under the microscope into a series of varieties and types. These types are based upon the recognition of five main sources of tourmaline in sediments: granitic, pegmatitic, metamorphic injected, sedimentary authigenic, and reworked sedimentary detrital. Actual examples of the application of these concepts to the solution of problems of correlation, interpretation, and differentiation of sediments and to the reconstruction of paleogeographic conditions are given.
OpenAlex reports 126 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Tourmaline is really a complex isomorphous mineral group which can be easily differentiated under the microscope into a series of varieties and types. These types are based upon the recognition of five main sources of tourmaline in sediments: granitic, pegmatitic, metamorphic injected, sedimentary authigenic, and reworked sedimentary detrital. Actual examples of the application of these concepts to the solution of problems of correlation, interpretation, and differentiation of sediments and to the reconstruction of paleogeographic conditions are given.
Key concepts: Tourmaline, Authigenic, Geology, Pegmatite, Sedimentary rock, Group (periodic table), Geochemistry, Metamorphic rock