Yangtze and Cathaysia Blocks Assembled During the Early Cryogenian NeoProterozoic
Neoproterozoic
arc-related mafic–ultramafic rocks and syn-collision granite from the
western segment of the Jiangnan Orogen, South China: constraints on the
Neoproterozoic assembly of the Yangtze and Cathaysia Blocks
Authors:
Yao et al
Abstract:
The
Jiangnan Orogen is considered as the trace of the collisional suture
between the Yangtze and Cathaysia Blocks in South China. Here we
investigate the mafic-ultramafic suites and granitoids exposed in the
Yuanbaoshan area along the western segment of the Jiangnan Orogen. We
present new LA–ICP–MS zircon U–Pb data, Hf isotopes and whole rock
geochemistry from a suite of granite, gabbro diorite and
mafic–ultramafic rocks from this area. Zircons in the mafic rocks yield a
U–Pb age of 854.7 ± 5.3 Ma, whereas those from the granites show ages
of 822.6 ± 5.2, 830.7 ± 5.0, 823.8 ± 5.3 and 833.0 ± 5.9 Ma. The
Neoproterozoic mafic–ultramafic rocks display dominantly tholeiitic
features and are characterized by negative Ba, Nb, Ta, Zr, Hf and Sr
anomalies and LREE enriched patterns, with a minor negative Eu anomaly.
The gabbro diorite also exhibits similar geochemical characters. The
mafic suite plots in the field of volcanic arc basalt in tectonic
discrimination diagrams and displays distinctive geochemical signatures
of an arc setting. The zircons from these rocks show ɛHf(t) values in
the range of 3.9 to 13.8. The granitoids in northern Guangxi are typical
S–type granites with high ACNK values (1.15–1.40), and are classified
as collision–related granites in tectonic discrimination diagrams. The
zircons from these rocks show negative ɛHf(t) values of –18.99 to –0.84.
We correlate the granitoids with the continent–continent collisional
orogeny between the Yangtze and Cathaysia blocks. Our new results
suggest a ∼ 854 Ma volcanic arc and an 840–820 Ma collisional setting in
the western segment of the Jiangnan Orogen, which is different from
previous proposals of plume and bimodal magmatic settings and place the
timing of assembly of the Yangtze and Cathaysia Blocks at some time ca.
850-800 Ma
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