Hirnantian Isotope Carbon Excursion in Gorny Altai, southwestern Siberia
The Hirnantian Isotope Carbon Excursion (HICE), a glaciation-induced positive δ13C shift in the end-Ordovician successions, has been widely used in chemostratigraphic correlation of the Ordovician–Silurian boundary beds in many areas of the world. However, large regions with Ordovician sediments in...
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| Autors principals: | , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Estonian Academy Publishers
2015-08-01
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| Col·lecció: | Estonian Journal of Earth Sciences |
| Matèries: | |
| Accés en línia: | http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2015/issue_3/earth-2015-3-225-232.pdf |
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