气候变化领域集成服务门户(CCPortal): Mesozoic deposits of SW Gondwana (Namibia): unravelling Gondwanan sedimentary dispersion drivers by detrital zircon

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DOI	10.1007/s00531-020-01864-2
	Mesozoic deposits of SW Gondwana (Namibia): unravelling Gondwanan sedimentary dispersion drivers by detrital zircon
	Zieger J.; Harazim S.; Hofmann M.; Gärtner A.; Gerdes A.; Marko L.; Linnemann U.
发表日期	2020
ISSN	14373254
起始页码	1683
结束页码	1704
卷号	109 期号:5
英文摘要	The Namibian Mesozoic successions may be remnant of a high dynamic sedimentary system that is characterized by multiple stages of sediment accumulation and erosion with contemporaneous homogenization starting with the deposition of the Permo-Carboniferous Dwyka Group strata and continues at least until the Lower Cretaceous. The Lower Cretaceous sedimentary system is interpreted to have involved at least an area covering the whole SW Gondwana, documenting the sedimentary history during the evolution from an ice house environment to an arid desert. To test the sediment homogenization hypothesis, we applied a combination of isotopic and morphometric data on detrital zircon grains, as well as whole-rock geochemical data of selected Mesozoic sandstones from Namibia. As a base for the interpretation of the detrital zircon age data we compiled a zircon age dataset with c. 44,000 analyses for the southern African region. All samples reveal a major detrital pan-African zircon age peak of c. 0.5–0.7 Ga sourced from the pan-African magmatic events occurring around the Kalahari Craton margin. The lowermost Triassic is characterized by the occurrence of additional Mesoproterozoic and Paleoproterozoic age peaks of c. 1.0–1.2 Ga and 1.8–2.0 Ga with a majority of zircon grains showing angular shapes. The protosource of these grains is interpreted to possibly be the Namaqua Metamorphic Complex and other Paleoproterozoic structural units deformed in course of the Namaqua orogeny. In contrast, other samples show a prominent Permo-Triassic age peak and completely rounded zircon grains, putatively derived from within the Gondwanides volcanic arc. The disparity in the zircon age pattern may point towards a change in provenance and also a change in the whole system of zircon recycling during the Mesozoic southern Gondwana. The Lower Triassic Neu Loore fm. are constrained to more local bedrock sources and short zircon transport distance. In contrast, zircon grains of the Middle Triassic Omingonde, the Jurassic Etjo und the Cretaceous Twyfelfontein formations are an expression for a major recycling and sediment homogenization system. The system was facilitated by an interplay between fluvial and eolian sedimentary transport systems. © 2020, The Author(s).
英文关键词	Gondwana; Karoo; Mesozoic; Namibia; Zircon U–pb
语种	英语
scopus关键词	detrital deposit; dispersion; Gondwana; homogeneity; isotopic composition; Mesozoic; morphometry; sandstone; sediment chemistry; sediment transport; zircon; Namibia
来源期刊	International Journal of Earth Sciences
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/147659
作者单位	Senckenberg Museum für Naturkunde Görlitz, Am Museum 1, Görlitz, 02826, Germany; TU Dresden, Fakultät Umweltwissenschaften, Institut für Geographie, Helmholtzstr. 10, Dresden, 01069, Germany; Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Königsbrücker Landstr. 159, Dresden, 01109, Germany; Institut für Geowissenschaften, Mineralogie, Goethe Universität Frankfurt, Altenhoeferallee 1, Frankfurt, 60438, Germany
推荐引用方式 GB/T 7714	Zieger J.,Harazim S.,Hofmann M.,et al. Mesozoic deposits of SW Gondwana (Namibia): unravelling Gondwanan sedimentary dispersion drivers by detrital zircon[J],2020,109(5).
APA	Zieger J..,Harazim S..,Hofmann M..,Gärtner A..,Gerdes A..,...&Linnemann U..(2020).Mesozoic deposits of SW Gondwana (Namibia): unravelling Gondwanan sedimentary dispersion drivers by detrital zircon.International Journal of Earth Sciences,109(5).
MLA	Zieger J.,et al."Mesozoic deposits of SW Gondwana (Namibia): unravelling Gondwanan sedimentary dispersion drivers by detrital zircon".International Journal of Earth Sciences 109.5(2020).