2018
DOI: 10.1007/s12303-018-0026-z
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Neoproterozoic deposition and Triassic metamorphism of metasedimentary rocks in the Nam Co Complex, Song Ma Suture Zone, NW Vietnam

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Cited by 16 publications
(14 citation statements)
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“…The U -Pb isotopic compositions of zircon were plotted in the Tera -Wasserburg concordia and probability distribution diagrams (Figure . 3). Similar to the three metasandstone samples in Nam Co Complex reported by Hau et al, 2018, LA -MC -ICP -MS zircon age data from samples SM14 and SM20 show the major zircon age peak at ~800÷980 Ma and less important peaks at ~1600 Ma, ~1850 Ma and ~2500 Ma (Figure 4). The median 206 Pb/ 238 U ages of Neoproterozoic zircon population in two samples SM14 and SM20 were calculated as 855±20 Ma (2σ) and 940±16 Ma (2σ), respectively (Figures 4a, c).…”
Section: U -Pb Agessupporting
confidence: 77%
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“…The U -Pb isotopic compositions of zircon were plotted in the Tera -Wasserburg concordia and probability distribution diagrams (Figure . 3). Similar to the three metasandstone samples in Nam Co Complex reported by Hau et al, 2018, LA -MC -ICP -MS zircon age data from samples SM14 and SM20 show the major zircon age peak at ~800÷980 Ma and less important peaks at ~1600 Ma, ~1850 Ma and ~2500 Ma (Figure 4). The median 206 Pb/ 238 U ages of Neoproterozoic zircon population in two samples SM14 and SM20 were calculated as 855±20 Ma (2σ) and 940±16 Ma (2σ), respectively (Figures 4a, c).…”
Section: U -Pb Agessupporting
confidence: 77%
“…Three samples from the Nam Co Complex have been collected for zircon separation (Figure 2). Samples SM14 and SM20 are semi -pelitic rocks, consisting of quartz, muscovite, chlorite, and minute granite; sample SM09 is finegrained sandstone (Hau et al, 2018). The U -Th -Pb isotopic dating on the detrital zircon was carried out from two semi -pelitic samples (SM14 and SM20, Figure 2b), whereas Hf isotopic analysis was carried out from SM14, SM20 and SM09.…”
Section: Methodsmentioning
confidence: 99%
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