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How are diamictites dated? 


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Diamictites are dated using various methods such as U-Pb dating of detrital zircons found within the rocks. For instance, Late Ordovician diamictites in Turkey were dated using U-Pb dating of granitic pebbles, providing ages ranging from 576.5 to 964.6 Ma . Additionally, the youngest 206Pb/238U ages in diamictites from different regions were used to determine the age of detrital zircons transported mainly from the northern margin of Gondwana . Furthermore, the absence of enrichments in siderophile elements like Ir in South African diamictites suggests no impact origin, as these elements are typically abundant in meteorites but not in terrestrial rocks . These dating methods help establish the age and origin of diamictites in geological records.

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Diamictites can be dated using methods like γ-γ coincidence spectrometry to study possible meteoritical components, as done in the research on South African diamictites.
Diamictites are dated using Laser Ablation Inductively Coupled Plasma Mass Spectrometry U-Pb dating of detrital zircons, revealing ages of 499.1-562.5 Ma, indicating provenance from Gondwana's northern margin.
Diamictites are dated using methods like radiometric dating of associated volcanic rocks or by correlating with other dated rock layers, providing insights into their formation during specific geological time periods.
Diamictites are dated based on the Neoproterozoic period (c. 720-635 Ma) using stratigraphic analysis within rift basins, indicating tectonic controls rather than climatic influences.

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