Arid
DOI10.1007/s00531-020-01864-2
Mesozoic deposits of SW Gondwana (Namibia): unravelling Gondwanan sedimentary dispersion drivers by detrital zircon
Zieger, J.1; Harazim, S.2; Hofmann, M.3; Gaertner, A.3; Gerdes, A.4; Marko, L.4; Linnemann, U.3
通讯作者Zieger, J.
来源期刊INTERNATIONAL JOURNAL OF EARTH SCIENCES
ISSN1437-3254
EISSN1437-3262
出版年2020
卷号109期号:5页码:1683-1704
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.
英文关键词Zircon U-pb Mesozoic Gondwana Karoo Namibia
类型Article
语种英语
国家Germany
开放获取类型hybrid, Green Published
收录类别SCI-E
WOS记录号WOS:000528647000001
WOS关键词U-PB ZIRCON ; FORMATION KAROO SUPERGROUP ; BELT NW NAMIBIA ; SOUTH-AFRICA ; PARANA BASIN ; ION-PROBE ; LU-HF ; GEOCHEMICAL EVIDENCE ; BOTUCATU FORMATION ; IGNEOUS COMPLEX
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/314759
作者单位1.Senckenberg Museum Nat Kunde Gorlitz, Museum 1, D-02826 Gorlitz, Germany;
2.Tech Univ Dresden, Inst Geog, Fak Umweltwissensch, Helmholtzstr 10, D-01069 Dresden, Germany;
3.Senckenberg Nat Hist Sammlungen Dresden, Museum Mineral & Geol, Konigsbrucker Landstr 159, D-01109 Dresden, Germany;
4.Goethe Univ Frankfurt, Inst Geowissensch, Mineral, Altenhoeferallee 1, D-60438 Frankfurt, Germany
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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):1683-1704.
APA Zieger, J..,Harazim, S..,Hofmann, M..,Gaertner, 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),1683-1704.
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):1683-1704.
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