Titlebook: Geology of Southwest Gondwana; Siegfried Siegesmund,Miguel A. S. Basei,Sebastian Book 2018 Springer International Publishing AG, part of

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The Evolution of the Damara Orogenic System: A Record of West Gondwana Assembly and Crustal Responseness, accuracy and internal consistency, and to build crustal and tectonic models. For this summary of the Damara Orogenic System, two large-scale internally consistent relational data sets have been integrated: (1) age-calibrated deformation histories have been correlated across the whole system on

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The Stratigraphy and Structure of the Western Saldania Belt, South Africa and Geodynamic Implicationan fore-arc basin fill. Sedimentary facies suggest the presence of a volcanic arc in the east, succeeded in the west by metaturbidites of the inner fore-arc basin and deeper-water metapelitic successions in the northwest interpreted to form slope-apron deposits overlying the toe of the prim and faci

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Suturing Gondwana in the Cambrian: The Orogenic Events of the Final Amalgamationpaleocontinents. The collisional orogen pattern throughout both western and eastern Gondwana is similar, indicating that although Gondwana was built up by the convergence of distinct paleocontinents, their approximation might be orchestrated by global geodynamics. In SW Gondwana, the opening of .. 6

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Untangling the Neoproterozoic-Early Paleozoic Tectonic Evolution of the Eastern Sierras Pampeanas HiTG suites of the Sierras de Córdoba (T. 1.3–1.0 Ga). Achalian magmatism exhibits more radiogenic εNd. values (0.5 to −4) and T. ages younger than 1.3 Ga. Two types of Pampean-related mafic rocks are recognized: one with a depleted mantle signature and another younger group with an enriched mantle si

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ping, of the craton boundaries and associated terranes; major faults, structural lineaments and ring structures; specific features which have a geophysical expression, such as the Witwatersrand Basin, the Xade Complex and the tectonostratigraphic zones of the Damara-Ghanzi-Chobe Orogenic Belt; the N

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Kia Hays,Karen Jungblut,Stephen D. Smithoko and Dom Feliciano belts. The history of the southern Adamastor Ocean spans between 900 and 590 Ma, from the earliest records of magmatism related to Rodinia break-up (980–780 Ma), through the climax of the extensional phase that led to the opening of a vast ocean (780–640 Ma). Tectonic inversion