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Now showing items 9989-10008 of 43490
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(2006)Mesozoic volcanism is widespread throughout northeastern China, but precise geochronological constraints were previously lacking. Twenty samples, including basalt and basaltic andesites, from the Great Xing'an Range were ...
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(2003)Various settings took place during the Late Mesozoic: divergent, convergent, collisional, and transform. After mid-Jurassic collision of the Siberian and Chinese cratons, a latitudinal system of post-collision troughs ...
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(2001)The data on the successions of the Late Miocene - Pliocene mammalian faunas from the territory of the former Soviet Union and Mongolia are summarised. The main characteristics of the MN zone for these territories are given.
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(2006)The fossil teeth of land mammals offer a powerful tool to map the regional details of past climate change in the terrestrial realm. We use mean plant-eater hypsodonty (molar crown height) of late Neogene mammal localities ...
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LATE MIOCENE CLIMATE IN THE CIRCUM-ALPINE REALM-A QUANTITATIVE ANALYSIS OF TERRESTRIAL PALAEOFLORAS (2006)Selected mega- and microfloras from Central and Southern Europe have been analysed for the time interval Tortonian/Pannonian (MN 9-12) with the Coexistence Approach to obtain quantitative palaeoclimate data. The results ...
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(2006)A fish otolith assemblage from the Messinian 'Lago-mare' deposits of the Colombacci Formation cropping out in the Montecalvo in Foglia Syncline, Marche, central Italy, is described. The assemblage displays a low diversity ...
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(2006)The palaeogeographic evolution of the Paratethyan and Mediterranean realms are reconstructed with three maps ranging from the Late Miocene to the Middle-Late Pliocene. The maps are based on the facial analysis of selected ...
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(2001)The decade of scientific drilling and multidisciplinary studies of lacustrine sedimentary sequences on Lake Baikal has contributed greatly to expansion of our knowledge on the Asian continent response to global climate and ...
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(2002)Geochemical data on Late Cenozoic within-plate basalts from the southern part of the Russian Far East are utilized to demonstrate the main features of the lithospheric structure in the continent-ocean transition zone and ...
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(2006)Origin and tectonic setting of the late Neoproterozoic Dokhan Volcanics (ca. 610–560 Ma by whole rock Rb–Sr and ca. 600–590 Ma by SHRIMP U–Pb zircon) in the Egyptian Eastern Desert is debated. Debate concerns the tectonic ...
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(2006)An unusual late Neoproterozoic (c. 572 Ma) ophiolite is exposed in the Dariv Range (western Mongolia, which contains intermediate to acidic lavas and sheeted dykes, and an igneous layered complex consisting of gabbro-norites, ...
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(2006)The evolution of the basement of southern Madagascar north and south of the Ranotsara shear zone was investigated using (U + Th)/Pb electron probe monazite age dating in combination with petrographic constraints. Several ...
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(2006)The Cenozoic Tian Shan is one of the preeminent examples of an intracontinental orogen. However, there remains a significant controversy over when deformation related to the India-Asia collision commenced and therefore how ...
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(2006)Brachiopods from the late Ordovician (late Caradoc) Dulankara Formation of the Chu-Ili Range, Kazakhstan, are reviewed. Those from the upper two members of the formation, the Degeres and Akkol members, are systematically ...
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(2006)Most of Kazakhstan belongs to the central part of the Eurasian Paleozoic mobile belts for which previously proposed tectonic scenarios have been rather disparate. Of particular interest is the origin of strongly curved ...
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(2001)The results of a quantitative palynological analysis, emphasizing organic-walled dinoflagellate cysts (dinocysts), of Palaeocene–Eocene deposits exposed in the Sokolovsky Quarry (Turgay Trough, Northern Kazakhstan) are ...
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(2003)To further understand the distribution and abundance of Apectodinium through space and time, dinoflagellate cyst (dinocyst) records from two well-calibrated Paleogene sections in the Tethys (Tunisia and Uzbekistan) have ...
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(2006)Mafic dyke swarms and aulacogens are major anorogenic extensional events in the Late Paleoproterozoic North China Craton (NCC). The N-NNW mafic dyke swarms are widespread in the NCC, whose ages span between 1.83 and 1.77 ...
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(2004)The present kinematic and dynamic analysis of large-scale strike-slip faults, which enabled the formation of a collage of Altai terranes as a result of two collisional events. The Late Devonian–Early Carboniferous collision ...
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(2003)The cause of the late Paleozoic (ca. 355 255 Ma) ice age remains uncertain. A lowering of atmospheric carbon dioxide levels near the beginning of this time period occurred in response to the rise of land plants and likely ...
Now showing items 9989-10008 of 43490