Revised Tal Group lithostratigraphy and record of biostratigraphically significant from Mussoorie syncline, Lesser Himalaya
A succession of bedded earthy argillaceous dolomite (~17 m) overlain by earthy siltstone (~12 m) is recognised in the lower part of the Deo-Ka-Tibba Formation (Tal Group) in the northeastern limb of the Mussoorie syncline, near Bhusti village. The recognition of these two diagnostic units necessitat...
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| Главные авторы: | , , , , |
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| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
SAGE Publishing
2026-06-01
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| Серии: | Journal of the Palaeontological Society of India |
| Online-ссылка: | https://doi.org/10.1177/05529360251400420 |
| Метки: |
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