scholarly journals Supplemental Material: The assembly of the South China and Indochina blocks: Constraints from the Triassic felsic volcanics in the Youjiang Basin

2020 ◽  
Author(s):  
Chengshi Gan ◽  
Yuzhi Zhang ◽  
et al.
Keyword(s):  
South China ◽  
Middle Triassic ◽  
Volcanic Rocks ◽  
Icp Ms ◽  
O Isotopes ◽  
Youjiang Basin ◽  
Felsic Volcanic ◽  
Early Middle Triassic ◽  
Felsic Volcanic Rocks

Table S1: LA-ICP-MS zircon U-Pb dating results for Early-Middle Triassic felsic volcanic rocks in the Youjiang Basin; Table S2: In-situ zircon Hf-O isotopes results for Early-Middle Triassic felsic volcanic rocks in the Youjiang Basin; Table S3: Geochemical compositions for Early-Middle Triassic felsic volcanic rocks in the Youjiang Basin.

scholarly journals Supplemental Material: The assembly of the South China and Indochina blocks: Constraints from the Triassic felsic volcanics in the Youjiang Basin

2020 ◽  
Author(s):  
Chengshi Gan ◽  
Yuzhi Zhang ◽  
et al.
Keyword(s):  
South China ◽  
Middle Triassic ◽  
Volcanic Rocks ◽  
Icp Ms ◽  
O Isotopes ◽  
Youjiang Basin ◽  
Felsic Volcanic ◽  
Early Middle Triassic ◽  
Felsic Volcanic Rocks

Table S1: LA-ICP-MS zircon U-Pb dating results for Early-Middle Triassic felsic volcanic rocks in the Youjiang Basin; Table S2: In-situ zircon Hf-O isotopes results for Early-Middle Triassic felsic volcanic rocks in the Youjiang Basin; Table S3: Geochemical compositions for Early-Middle Triassic felsic volcanic rocks in the Youjiang Basin.

Post-collisional ca. 800 Ma A-type felsic volcanic rocks in the eastern Jiangnan orogen, South China

2020 ◽  
Vol 203 ◽  
pp. 104567
Author(s):  
Ji-Biao Zhang ◽  
Yan-Xue Liu ◽  
Xiao-Zhong Ding ◽  
Heng Zhang ◽  
Chuan-Heng Zhang
Keyword(s):  
South China ◽  
Volcanic Rocks ◽  
Felsic Volcanic ◽  
Felsic Volcanic Rocks

Geochemistry and Isotope Composition of Paleoproterozoic Granites and Felsic Volcanics of the Elash Graben: Evidence of the Heterogeneity of the Early Precambrian Crust

2021 ◽  
Vol 62 (10) ◽  
pp. 1175-1187
Author(s):  
A.D. Nozhkin ◽  
O.M. Turkina ◽  
K.A. Savko
Keyword(s):  
Isotope Composition ◽  
Volcanic Rocks ◽  
Rare Metal ◽  
Temporal Association ◽  
Metal Deposit ◽  
Wide Range ◽  
Rare Metal Deposit ◽  
Geochronological Study ◽  
Felsic Volcanic ◽  
Felsic Volcanic Rocks

Abstract —The paper presents results of a petrogeochemical and isotope–geochronological study of the granite–leucogranite association of the Pavlov massif and felsic volcanics from the Elash graben (Biryusa block, southwest of the Siberian craton). A characteristic feature of the granite–leucogranites is their spatial and temporal association with vein aplites and pegmatites of the East Sayan rare-metal province. The U–Pb age of zircon from granites of the Pavlov massif (1852 ± 5 Ma) is close to the age of the pegmatites of the Vishnyakovskoe rare-metal deposit (1838 ± 3 Ma). The predominant biotite porphyritic granites and leucogranites of the Pavlov massif show variable alkali ratios (K2O/Na2O = 1.1–2.3) and ferroan (Fe*) index and a peraluminous composition; they are comparable with S-granites. The studied rhyolites of the Tagul River (SiO2 = 71–76%) show a low ferroan index, a high K2O/Na2O ratio (1.6–4.0), low (La/Yb)n values (4.3–10.5), and a clear Eu minimum (Eu/Eu* = 0.3–0.5); they are similar to highly fractionated I-granites. All coeval late Paleoproterozoic (1.88–1.85 Ga) granites and felsic volcanics of the Elash graben have distinct differences in composition, especially in the ferroan index and HREE contents, owing to variations in the source composition and melting conditions during their formation at postcollisions extension. The wide range of the isotope parameters of granites and felsic volcanic rocks (εNd from +2.0 to –3.7) and zircons (εHf from +3.0 to +0.8, granites of the Toporok massif) indicates the heterogeneity of the crustal basement of the Elash graben, which formed both in the Archean and in the Paleoproterozoic.

The Duck Pond and Boundary Cu–Zn deposits, Newfoundland: new insights into the ages of host rocks and the timing of VHMS mineralization

2010 ◽  
Vol 47 (12) ◽  
pp. 1481-1506 ◽  
Author(s):  
Vicki McNicoll ◽  
Gerry Squires ◽  
Andrew Kerr ◽  
Paul Moore
Keyword(s):  
Volcanic Rocks ◽  
Sedimentary Rocks ◽  
Isotopic Data ◽  
Sulphide Ores ◽  
Intrusive Rocks ◽  
Felsic Volcanic ◽  
Host Rocks ◽  
Felsic Volcanic Rocks

The Duck Pond Cu–Zn–Pb–Ag–Au deposit in Newfoundland is hosted by volcanic rocks of the Cambrian Tally Pond group in the Victoria Lake supergroup. In conjunction with the nearby Boundary deposit, it contains 4.1 million tonnes of ore at 3.3% Cu, 5.7% Zn, 0.9% Pb, 59 g/t Ag, and 0.9 g/t Au. The deposits are hosted by altered felsic flows, tuffs, and volcaniclastic sedimentary rocks, and the sulphide ores formed in part by pervasive replacement of unconsolidated host rocks. U–Pb geochronological studies confirm a long-suspected correlation between the Duck Pond and Boundary deposits, which appear to be structurally displaced portions of a much larger mineralizing system developed at 509 ± 3 Ma. Altered aphyric flows in the immediate footwall of the Duck Pond deposit contained no zircon for dating, but footwall stringer-style and disseminated mineralization affects rocks as old as 514 ± 3 Ma at greater depths below the ore sequence. Unaltered mafic to felsic volcanic rocks that occur structurally above the orebodies were dated at 514 ± 2 Ma, and hypabyssal intrusive rocks that cut these were dated at 512 ± 2 Ma. Some felsic samples contain inherited (xenocrystic) zircons with ages of ca. 563 Ma. In conjunction with Sm–Nd isotopic data, these results suggest that the Tally Pond group was developed upon older continental or thickened arc crust, rather than in the ensimatic (oceanic) setting suggested by previous studies.

Sign in / Sign up

Export Citation Format

Share Document