About Lüliang new rock drill
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6 FAQs about [Lüliang new rock drill]
How old is a zircon rock in the Lüliang group?
Four samples from the metamorphic volcanic rocks of the Lüliang Group were analyzed using the Sm–Nd isochron dating method and defined an isochron age of 2351 ± 56 Ma with the corresponding initial 143 Nd/ 144 Nd ratio of 0.50958 ± 5 and ɛ Nd (t) of −0.3 ± 0.5 (Geng et al., 2000), which is slightly older than the ∼2.2 Ga zircon age of this study.
What are the rough ages of the Lüliang group?
Three rough ages were reported for the metavolcanic rocks of the Lüliang Group, including a whole rock Sm–Nd isochron age of 2360 ± 95 Ma (Geng et al., 2000), and single-grained zircon U–Pb ages of 2051 ± 68 Ma and 2099 ± 41 Ma (Yu et al., 1997).
Which granitoids are found in Lüliang complex?
In this study, we present a comprehensive analysis of the late Neoarchean to Paleoproterozoic granitoids within the Lüliang Complex, including whole-rock major and trace element compositions, secondary ion mass spectrometry (SIMS) zircon U–Pb geochronology, and in-situ zircon Hf–O isotopes.
Was the Lüliang complex metamorphosed in the Paleoproterozoic?
These new ages, integrated with recently reported U–Pb zircon ages for the Jiehekou Group and Paleoproterozoic granitoids, suggest that all of the lithological assemblages of the Lüliang Complex formed and were metamorphosed in the Paleoproterozoic, not in the Neoarchean.
Where is the Lüliang complex located?
The Lüliang Complex is situated in the central section of the TNCO and includes various late Neoarchean to Paleoproterozoic granitoid plutons and meta-supracrustal rocks.
Where is the Lüliang group located?
The Lüliang Group is distributed in the central part of the PLC and comprises greenschist- to amphibolite-facies metamorphosed sedimentary rocks with banded iron formation (BIF) in the lower sequence and metamorphosed volcanic rocks (e.g. basalt, andesite and dacite) in the upper part (Yu et al., 1997).