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The Evolution of the Rheic Ocean
Geological evolution of middle to late Paleozoic rocks in the Avalon terrane of northern mainland Nova Scotia, Canadian Appalachians: a record of tectonothermal activity along the northern margin of the Rheic Ocean in the Appalachian-Caledonide orogen.
Special Papers
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Geology and Geodynamic Development of Uganda with Explanation of the 1:1,000,000 Scale Geological Map
This Special Paper describes an update of the geology and geodynamic development of Uganda. It is based on extensive work that a Consortium, headed by the Geological Survey of Finland (GTK), has executed in close cooperation with the Department of Geological Survey and Mines (DGSM) in Uganda during 2008-2012. The publication is compiled by a team of experts, based on a uniform database, and gives a coherent geological and geodynamic model for the whole country and, at the same time, it is an explanation to the new 1:1 million scale geological map of Uganda. Geologically Uganda is divided into a number of tectono-thermal domains, often closely related to continental scale "building blocks", e...
Problems of Geocosmos—2022
Problems of Geocosmos conference proceedings series provide a snapshot of current research in a broad area of Earth Sciences carried out in Russia and elsewhere. Themes covered include solar physics, physics of magnetosphere, ionosphere and atmosphere, solar-terrestrial coupling links, seismology and geodynamics, paleomagnetism and rock magnetism, as well as cross-disciplinary studies. The proceedings are carefully edited, providing a panoramic outlook of a broad area of Earth Sciences. The readership includes colleague researchers, students and early career scientists. The proceedings will help the readers to look at their research fields from various points of view. Problems of Geocosmos conferences are held by Earth Physics Department, St. Petersburg University bi-annually since 1994. It is one of the largest forums of this kind in Russia/former Soviet Union attracting up to 200 researchers in Earth and magnetospheric physics.
