<--- Back to Details
First PageDocument Content
Hypsodont / Geology / Molar / Ungulate / Miocene / Mikael Fortelius / Peridotite / Elasmotherium
Date: 2002-05-29 14:28:42
Hypsodont
Geology
Molar
Ungulate
Miocene
Mikael Fortelius
Peridotite
Elasmotherium

letters to nature serpentinized peridotite (Fig. 2c). Assuming a lower-crustal velocity of 3.6 km s21, the estimated maximum S-velocity perturbation of 10% near the wedge corner could represent a level of serpentinizatio

Add to Reading List

Source URL: www.biocenter.helsinki.fi

Download Document from Source Website

File Size: 319,27 KB

Share Document on Facebook

Similar Documents

Palaeobio Palaeoenv:71–82 DOIs12549ORIGINAL PAPER  Perissodactyla from the late Middle Miocene Gratkorn

Palaeobio Palaeoenv:71–82 DOIs12549ORIGINAL PAPER Perissodactyla from the late Middle Miocene Gratkorn

DocID: 1uxib - View Document

Miocene snakes from northeastern Kazakhstan: new data on the evolution of snake assemblages in Siberia

Miocene snakes from northeastern Kazakhstan: new data on the evolution of snake assemblages in Siberia

DocID: 1umvo - View Document

The Late Miocene climate response to a modern Sahara desert

The Late Miocene climate response to a modern Sahara desert

DocID: 1uivs - View Document

Supplementary notes Böhme, M., Ilg, A., Winklhofer, M. Late Miocene “washhouse” climate in Europe 1. Stratigraphic-chronological framework Locality

Supplementary notes Böhme, M., Ilg, A., Winklhofer, M. Late Miocene “washhouse” climate in Europe 1. Stratigraphic-chronological framework Locality

DocID: 1u2JX - View Document