| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6442785 | Earth-Science Reviews | 2016 | 407 Pages |
Abstract
Kaolin is not only a raw material for one of the finest products, porcelain, but also a type mineral for a varied spectrum of environments of deposition characterized by a rather sharp upper limit of formation of 390 ± 10 °C at a pressure of 2000 bar. For all geoscientists dealing with processes below this physical-chemical boundary, the role of kaolin and its mineralogical constituents as marker cannot be overestimated.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Harald G. Dill,