The Hagendorf-Pleystein Province: the Center of Pegmatites in an Ensialic Orogen
The geological history of the HPPP, however, goes much further than the Carboniferous-Permian magmatic activity, when the last structural disturbances of the Variscan orogeny affected the NE-Bavarian Basement between 450 and 330 Ma. During this time mafic magmatic rocks together with sedimentary roc...
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| Format: | eBook |
| Language: | English |
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Cham
Springer International Publishing
2015, 2015
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| Edition: | 1st ed. 2015 |
| Series: | Modern Approaches in Solid Earth Sciences
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| Subjects: | |
| Online Access: | |
| Collection: | Springer eBooks 2005- - Collection details see MPG.ReNa |
Table of Contents:
- Geological and geographic setting of the HPPP
- Geology and lithology of the pegmatites, aplites, dykes and granites of the HPPP
- Mineralogy of the pegmatites, aplites, dykes and granites of the HPPP
- Pegmatites and aplites of the HPPP and adjacent mineral deposits along the western edge of the BM
- The readout of the pegmatites and aplites of the HPPP in regional surveys
- The physical-chemical regime during formation and alteration of the pegmatites and aplites
- Synopsis – the evolution of pegmatites and aplites of the HPPP
- Summary and outlook on phosphate pegmatites worldwide