Age relations for assembly of Gondwana and Pangea indicate that the timing of collisional
orogenesis between amalgamating continental bodies was synchronous with subduction …

Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by
Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude “ …

Дано описание геологии Южного и Среднего Урала, облеченное в концентрированную
форму геодинамического анализа. В книге охарактеризована структура Урала, а также …

Книга представляет собой первое сводное монографическое описание палеозойского
интрузивного магматизма Урала. Изложены результаты авторских разработок, на …

The Phanerozoic history of the Paleo-Asian, Tethyan, and Pacific oceanic domains is
important for unraveling the tectonic evolution of the Eurasian and Laurentian continents …

The Southern Urals of Russia contain what is arguably one of the best-preserved examples
of an arc–continent collision in any Paleozoic orogen. The arc–continent collision history …

We present a summary of geophysical models of the subcrustal lithosphere of Europe. This
includes the results from seismic (reflection and refraction profiles, P-and S-wave …

The Dom Feliciano Belt, situated in southernmost Brazil and Uruguay, contains a large mass
of granite–gneissic rocks (also known as Florianópolis/Pelotas Batholith) formed during the …

The northern border of the Variscan Moroccan Meseta is characterized by the presence of
Cambrian rocks affected by pre-Variscan deformation (the Sehoul block) thrust to the south …

Murzinka and Dzhabyk are continental-type batholiths of the middle and southern East
Uralian domain. They comprise mainly undeformed peraluminous K-rich granites whose …