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- aggregation classification "A1".
- aggregation creator B510058.
- aggregation creator B510059.
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- aggregation creator person.
- aggregation creator person.
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- aggregation creator person.
- aggregation date "2011".
- aggregation format "application/pdf".
- aggregation hasFormat 1908601.bibtex.
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- aggregation isPartOf urn:issn:0954-4879.
- aggregation language "eng".
- aggregation rights "I have transferred the copyright for this publication to the publisher".
- aggregation subject "Earth and Environmental Sciences".
- aggregation title "Emplacement and exhumation of the Kuznetsk-Alatau basement (Siberia): implications for the tectonic evolution of the Central Asian Orogenic Belt and sediment supply to the Kuznetsk, Minusa and West Siberian Basins".
- aggregation abstract "New geochronological data [zircon U/Pb, titanite fission-track (TFT) and apatite fission-track (AFT) dating and apatite (U-Th-Sm)/He thermochronology] and thermal history modelling yield constraints on the development of the granitoid basement of the Kuznetsk-Alatau Mountains, southern Siberia. The final stages of magmatism in the Kuznetsk-Alatau palaeo-island-arc are Late Cambrian, and collision of the arc with Siberia occurred in the Early Ordovician. The basement was exhumed by the Early Devonian. Continuous Devonian-Early Triassic sedimentation filled the adjoining Kuznetsk and Minusa basins and buried (and re-heated) the Kuznetsk-Alatau basement. After initial Pangaea break-up and Siberian flood-basalt magmatism, the basement reached TFT and AFT retention-temperatures in the Middle Triassic and Early Cretaceous, respectively, during denudation-induced cooling.".
- aggregation authorList BK854862.
- aggregation endPage "256".
- aggregation issue "4".
- aggregation startPage "248".
- aggregation volume "23".
- aggregation aggregates 1909793.
- aggregation isDescribedBy 1908601.
- aggregation similarTo j.1365-3121.2011.01006.x.
- aggregation similarTo LU-1908601.