| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699168 | Chemical Geology | 2012 | 12 Pages |
Abstract
⺠The Mottled Zone Event was a spontaneous combustion of bituminous chalks and marls. ⺠This resulted in the formation of high-T low-P metamorphic mineral assemblages. ⺠On a sufficiently large scale (100-102 m) the metamorphic process was isochemical. ⺠Isochemistry is most convincingly demonstrated on isocon plots. ⺠On a < 1 m scale intensive veining indicates mobilization of several elements.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Y.I. Geller, A. Burg, L. Halicz, Y. Kolodny,