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Liangchahe Granodiorite

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Journal Article
Journal: GSA Bulletin
Published: 06 July 2020
GSA Bulletin (2021) 133 (3-4): 523–538.
... in their source. In combination with moderate zircon saturation temperatures (814–822 °C), we infer that the Tieyupu granodiorites were formed by melting of Neoproterozoic metabasites under high-pressure (>1.5 GPa) and moderate-temperature (HP-MT) conditions. The Liangchahe granodiorites (415 ± 8 Ma) also...
FIGURES | View All (12)
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Laser ablation–multicollector–inductively coupled plasma–mass spectrometry (LA-MC-ICP-MS) U-Pb concordia diagrams for the Paleozoic granites from the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]). MSWD—mean square of weighted deviates.
Published: 06 July 2020
Figure 4. Laser ablation–multicollector–inductively coupled plasma–mass spectrometry (LA-MC-ICP-MS) U-Pb concordia diagrams for the Paleozoic granites from the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]). MSWD—mean square of weighted deviates.
Image
(A–C) Chondrite-normalized rare earth element (REE) patterns and (D–F) primitive mantle (PM)–normalized trace-element spider diagrams for the Paleozoic granites from the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]). Chondrite and primitive mantle values are from Sun and McDonough (1989). N-MORB—normal mid-ocean-ridge basalt.
Published: 06 July 2020
Figure 6. (A–C) Chondrite-normalized rare earth element (REE) patterns and (D–F) primitive mantle (PM)–normalized trace-element spider diagrams for the Paleozoic granites from the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]). Chondrite
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(A–C) Cathodoluminescence (CL) images for the Paleozoic granites from the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]). Circles indicate the location of laser ablation–multicollector–inductively coupled plasma–mass spectrometry (LA-MC-ICP-MS) Hf analyses, where the numbers in circles refer to the εHf(t) values. All εHf(t) values of the granites were calculated according their crystallization age.
Published: 06 July 2020
Figure 3. (A–C) Cathodoluminescence (CL) images for the Paleozoic granites from the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]). Circles indicate the location of laser ablation–multicollector–inductively coupled plasma–mass spectrometry (LA
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(A) A/NK [Al2O3/(Na2O + K2O)] vs. A/CNK [molar ratio Al2O3/(CaO + Na2O + K2O)], (B) quartz–alkali feldspar–plagioclase (Q-A-P), (C) SiO2–FeO/(FeO + Mg), and (D) SiO2– (Na2O + K2O-CaO) (after Frost et al., 2001) diagrams for the Paleozoic granites from the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]).
Published: 06 July 2020
the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]).