Results 191 to 200 of about 3,614 (211)
Some of the next articles are maybe not open access.

Chapter 6.4 The Oldest Rock Assemblages of the Siberian Craton

2007
Publisher Summary This chapter elaborates the oldest rock assemblages of the Siberian Craton. The Siberian Craton that occupies an area of approximately 4 × 10 6 km 2 is overlain largely by Mesoproterozoic to Phanerozoic sedimentary rocks, whose thickness ranges between 1 and 8 km, averaging approximately 4 km.
Oleg M. Rosen, O.M. Turkina
openaire   +1 more source

Phanerozoic mafic magmatism in the southern Siberian craton: geodynamic implications

Russian Geology and Geophysics, 2010
Abstract The Phanerozoic history of mafic magmatism in the southern Siberian craton included three major events. The earliest event (∼500 Ma) recorded in dolerite dikes occurred during accretion and collision at the early stage of the Central Asian orogen.
Gladkochub, D.   +6 more
openaire   +2 more sources

Proterozoic mafic magmatism in Siberian craton: An overview and implications for paleocontinental reconstruction

Precambrian Research, 2010
Sergei A Pisarevsky   +2 more
exaly  

Home - About - Disclaimer - Privacy