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Formation and Crust-Mantle Geodynamic Processes of the Neoarchean K-rich Granitoid Belt in the Southern Range of Eastern Hebei-Western Liaoning Provinces, North China Craton - Neoarchean K-rich Granitoid Belt in the Northern North China Craton (Hardcover, 1st ed. 2022)
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Formation and Crust-Mantle Geodynamic Processes of the Neoarchean K-rich Granitoid Belt in the Southern Range of Eastern Hebei-Western Liaoning Provinces, North China Craton - Neoarchean K-rich Granitoid Belt in the Northern North China Craton (Hardcover, 1st ed. 2022)
Series: Springer Theses
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Meso- to Neoarchean is a critical transitional period for the
formation and evolution of continental crust and the corresponding
geodynamic mechanisms, during which the average composition of
continental crust gradually shifted from Na-enriched to K-enriched.
However, the ultimate source of K and its enrichment mechanism in
continental crust are still enigmatic. Moreover, fierce
controversies remain on the Precambrian subdivision and late
Archean geodynamic models of the North China Craton (NCC). Archean
basement terranes in the Eastern Hebei-Western Liaoning Provinces,
northern NCC display characteristic lithological zonation similar
to those developed in modern convergent plate margins, and from
northwest to southeast can be subdivided into the MORB-type
tholeiite belt, oceanic arc tectonic belt, and K-rich granitoid
belt. This book reports systematic field geological, petrographic,
structural, whole-rock geochemical, and zircon U-Pb-Hf-O isotopic
data for the various late Neoarchean lithological assemblages of
the K-rich granitoid belt. Their deformational characteristics and
petrogenesis are discussed in detail, and integrated with their
spatiotemporal relationships and metamorphic features, a late
Neoarchean active continental margin setting with multi-stage
trench retreats and subsequent arc-continent collision is proposed
to account for the formation and evolution of the K-rich granitoid
belt. It also throws light upon the ultimate source and enrichment
mechanism of K in the late Archean continental crust by comparing
K-rich granitoid belt with the adjacent oceanic arc tectonic belt.
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