Incipient formation of the African precursor basin to the Ediacaran-Cambrian Araçuaí − West Congo Orogen: Implications for Columbia breakup and Gondwana assembly
J. De Grave , S. Glorie , D.B. Archibald , L. Tack , D. Baudet , K. Theunissen , P. Nseka-Mbemba , A. Love-Pay
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引用次数: 0
Abstract
The Panafrican West Congo Belt (WCB) is part of the Ediacaran-Cambrian Araçuaí – West Congo Orogen (AWCO). The central part of the WCB is characterized by an ENE-verging fold-and-thrust belt with eastward decreasing deformation and metamorphic grade. It is underlain by c. 2.1 Ga Eburnean-aged rocks, that, in the study area (Lower Congo region, Democratic Republic of Congo, DRC), are represented by the Kimeza Basement Complex covered by the West Congo Supergroup. New mapping, field data, and detrital zircon chronology, constrain the maximum deposition of its basal Matadi Formation to c. 1.13 Ga. The previously considered basal Palabala Formation comprises mylonites derived from various protoliths from the underlying basement (Kimeza gneiss, Mpozo syenite), as well as Matadi metaquartzite, marking Palabala a tectono-structural unit between the Kimeza basement and Matadi Formation, giving rise to a revised lithostratigraphy. The Matadi Formation in the Lower Congo region is intruded by several (per)alkaline granites, such as the Noqui granite near Matadi and the Mao granite near Boma. New zircon U-Pb and Pb-Pb ages constrain these intrusions to c. 1.0 Ga (i.e. between 1008 ± 10 and 990 ± 10 Ma). We demonstrate that the Noqui peralkaline pluton, contrary to previous models, is unrelated to the adjacent Mpozo syenomonzonite for which we provide new ages of c. 1.95 to 1.99 Ga. The Kimeza basement that hosts the intrusions yielded a zircon Pb-Pb age of 2036 ± 8 Ma. Our data suggests a continuous supradetachment precursor basin to the AWCO, comprising the Brazilian Espinhaço (west) and Matadi deposits (east). Overstretching of the basement produced the (per)alkaline intrusions described here and corresponds to one of the successive extensional events (“E4”) that marks the protracted Columbia breakup history, preceding the building of the AWCO during Gondwana assembly.
期刊介绍:
Gondwana Research (GR) is an International Journal aimed to promote high quality research publications on all topics related to solid Earth, particularly with reference to the origin and evolution of continents, continental assemblies and their resources. GR is an "all earth science" journal with no restrictions on geological time, terrane or theme and covers a wide spectrum of topics in geosciences such as geology, geomorphology, palaeontology, structure, petrology, geochemistry, stable isotopes, geochronology, economic geology, exploration geology, engineering geology, geophysics, and environmental geology among other themes, and provides an appropriate forum to integrate studies from different disciplines and different terrains. In addition to regular articles and thematic issues, the journal invites high profile state-of-the-art reviews on thrust area topics for its column, ''GR FOCUS''. Focus articles include short biographies and photographs of the authors. Short articles (within ten printed pages) for rapid publication reporting important discoveries or innovative models of global interest will be considered under the category ''GR LETTERS''.