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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.]()
![(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.]()
![(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.]()
![(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]).]()
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Tieyupu Granodiorite
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Journal Article
Thermotectonic evolution of the Paleozoic granites along the Shangdan suture zone (central China): Crustal growth and differentiation by magma underplating in an orogenic belt Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 06 July 2020
GSA Bulletin (2021) 133 (3-4): 523–538.
..., suggesting a crustal thinning process. The Tieyupu granodiorites (437 ± 4 Ma) display Na-rich adakite affinity, i.e., SiO 2 = 69.1–70.1 wt%, Na 2 O/K 2 O = 1.9–2.26, positive zircon ε Hf( t ) values (+4.29 to +12.04), and high Sr/Y (137–160) and Y/Yb (9.89–10.25) ratios, implying a garnet-rich residue...
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Image
![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.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/gsabulletin/133/3-4/10.1130_B35466.1/3/s_523f4.png?Expires=2147483647&Signature=S8ww80sFcctPKZKV4AQ~0ogcpehcj3bF85EbU8DbRgM28XDmpsUsKQ3zba-uBTPlH52IeN2szm54tR6hyD78Q~VdH1Cm-WPOAjv1TeUcu71lc9gsoKQ6ZDwzmeRc7z4AlTrf4Q6FJCVvIufAhXfa8nBqiT~NKh07L5y0YmHGgHenJ1L9xC0hNpFciCUl3Rl7MCL-vRLQPXSENlARlRDCbi-a0H3fBC2J7hfgMvubhwnKE5~ZL-g3eqn4QV1eTxaodcNDUQGlnyboFe~HgUFUGdw3pTr3FYk2Uu5BEy9a2MvUw96RIrZElhidKUDBZ9I8Kz6kavlVrw8cMQ~qBSeTuw__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Laser ablation–multicollector–inductively coupled plasma–mass spectrometry ... Available to Purchase
in Thermotectonic evolution of the Paleozoic granites along the Shangdan suture zone (central China): Crustal growth and differentiation by magma underplating in an orogenic belt
> GSA Bulletin
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.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/gsabulletin/133/3-4/10.1130_B35466.1/3/s_523f6.png?Expires=2147483647&Signature=Nba-LzRQixjR4bCRgEe4n85FBqLHiGbxWpKn8nwLev03EIaw5m38jaXjEO3hEW7QRZb7KBztKbWfFos7CxLqdhl-ikO0GgOiR3y-Ih9bfWiYxxual4T-yx82UBOQ6JuJCWl55XYrkAH35gQkW4PDJeNM5E7Ue0dv2DVH~ldCMPZ4HcIL6b9QY~kg5EvYCCvOCrVVlygwk~~~7AZBi96LfdD48bYwPMFq7az8fIAOzUmy9E1xIV1UwZaDZY6gi91wvoKi1PZq8IJF-fTvjFKGmq715LaiaxfrrcR-VmHI91ugzlJtx7gzveRIDlv-qeF4CnDv4IVw4SYbIioNuTcxXA__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
(A–C) Chondrite-normalized rare earth element (REE) patterns and (D–F) prim... Available to Purchase
in Thermotectonic evolution of the Paleozoic granites along the Shangdan suture zone (central China): Crustal growth and differentiation by magma underplating in an orogenic belt
> GSA Bulletin
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
Image
![(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.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/gsabulletin/133/3-4/10.1130_B35466.1/3/s_523f3.png?Expires=2147483647&Signature=UOuTHrQhQhdicglyi-XdEVGSU~3OGY3HPE~m5AKeSgFIFapM28L8CM8oQkxrOktDKv3IXDYLXXQVV5~DwLvxGYmSnbhGv~tU0~rZnKopLYdxt9nzAMkmdhT4sAv8t-bwaXctSZtlmxkc0ijS4qbYYCH3kt95nxQ7Tp-W0cCEIAXdonEcst6VJLXRbykcrdU7Rrjj7VqJO8ijSS43fj93vBpiKfqLkmdjbzZtluBGO0zCx3CkXtD1JxcBqLb54OJMdN~hZJHu53WcRgh3kSHXU0dFn2S3KV6itrOUQsgmjzIyXRvHDdta07uTkYbyis5CBCBw7vuP-E0NIssuwYsAWQ__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
(A–C) Cathodoluminescence (CL) images for the Paleozoic granites from the D... Available to Purchase
in Thermotectonic evolution of the Paleozoic granites along the Shangdan suture zone (central China): Crustal growth and differentiation by magma underplating in an orogenic belt
> GSA Bulletin
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
Image
![(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]).](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/gsabulletin/133/3-4/10.1130_B35466.1/3/s_523f5.png?Expires=2147483647&Signature=j0bgLjFJQ-TsDwB0refBNTX~9rYsP5qqjTDQXr7pO7mm3jQiMhCqOxyVFHi8T3Xwxc3nnDA6~WLzEZ2yAq8wNjJODEXNS4Nnz0ZciJ0RreHdm-TrXn3Uffqs4KCF3-Hdbg7DNFBo7K8OEHxcNZCLnLqRG6fxKRFF~bqsEjZhqaQhlnkwOImIGj8hmR2GNjwTkFiyvY5htRZoaXny1ilL7Yg4BKuBjeWLb2Qf8qrTpWiHcQW96sO0K~qiPUXJxOEVM52ZiovjB11mWJ5LhlGEDJVlu~X-DSZwAqUO9AjJePFdKw1eCyQELUGSl6nF4FiFIQGhXhJHxte5bjvymYVuYg__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
(A) A/NK [Al 2 O 3 /(Na 2 O + K 2 O)] vs. A/CNK [molar ratio Al 2 O 3 /(CaO... Available to Purchase
in Thermotectonic evolution of the Paleozoic granites along the Shangdan suture zone (central China): Crustal growth and differentiation by magma underplating in an orogenic belt
> GSA Bulletin
Published: 06 July 2020
the Danfeng area (Tieyupu granodiorite [TYP], Liangchahe granodiorite [LXH], Yaogou monzogranite [YG]).
