Results 131 to 140 of about 77,436 (299)

Rhinocerotidae of the lower Miocene [PDF]

open access: yesAmerican Journal of Science, 1908
openaire   +1 more source

Ruminant macroevolution: a phylogenetic approach based on extant faunas [PDF]

open access: yes, 2013
Cantalapiedra, Juan L.   +2 more
core   +1 more source

Lower Miocene (Gaj) Fauna from Travancore-Cochin, South India

open access: yesJournal of the Palaeontological Society of India, 1958
M. R. Sahni, M. V. A. Sastry
doaj   +1 more source

New insights into tragulid phylogeny of Europe: Dorcatherium naui from the latest Middle Miocene of Austria [PDF]

open access: yes, 2013
Aiglstorfer, Manuela   +3 more
core   +1 more source

Dental eruption in ruminants and other mammals [PDF]

open access: yes, 2013
Asher, Robert J., Wörheide, Gert
core   +1 more source

Progressively Fenitised Schist and Carbonatitic Clasts From a Metasomatic Aureole Beneath the Alkalic Dunedin Volcano, Otago, New Zealand

open access: yesNew Zealand Journal of Geology and Geophysics, Volume 69, Issue 2, June 2026.
Clasts of albite‐porphyroblastic quartzofeldspathic schist, derived from the Otago Schist basement, occur within the Port Chalmers Breccia, a diatreme at the centre of the Dunedin stratovolcano, New Zealand. Schists have undergone varying degrees of replacement reactions (at temperatures of 300° to >500°C) producing hornfelses, with Ca‐ and K‐enriched ...
Alan F. Cooper
wiley   +1 more source

The Occurrence and Morphology of Naturally Occurring Respirable Mordenite Mineral Fibres in New Zealand

open access: yesNew Zealand Journal of Geology and Geophysics, Volume 69, Issue 2, June 2026.
Mordenite is a naturally occurring zeolite mineral that is the seventh most common zeolite mineral globally, forming at low temperatures (≥100°C) in hydrothermal systems. In New Zealand, extensive deposits of mordenite are commonly associated with areas of hydrothermal alteration, particularly in the Coromandel and Taupo Volcanic Zones.
Ayrton R. Hamilton   +6 more
wiley   +1 more source

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