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Differentiating magmatic doming and low-angle normal faulting remains critical for fully understanding the thermal, mechanical and chemical evolution of continental landmasses under extension. This zircon U–Pb dating and geochemical study documents two Middle to Late Jurassic batholiths (Lüshan and Haitangshan) from the Yiwulüshan range of western Liaoning, North China Craton. They consist of a variety...
The appinite–granite suite commonly occurs within post-subduction regimes during the final stage of an orogeny and thus holds the key to monitoring critical geodynamic and crustal evolutionary processes. The present zircon U–Pb dating and geochemical study documents the Late Permian appinite–granite complex from northwestern Liaoning, North China Craton. The hornblende-rich appinitic rocks have an...
The diversity exhibited by ferroan granitoids testifies to multiple distinct crustal and mantle processes generally within extensional environments and thus holds the key to monitoring important geodynamic and crustal evolutionary processes and calibrating terrane tectonic affinity. This study documents three Middle to Late Triassic ferroan granitoid suites from northwestern Liaoning, North China,...
Zircon U–Pb and hornblende 40 Ar/ 39 Ar dating document an Early Permian emplacement time for the Hercynian Guyang batholith from the northern margin of the North China Craton (NCC), with a variety of lithologies including: gabbro–gabbroic diorite–leuconorite, diorite and granodiorite, microgranular magmatic enclaves (MME), mafic dyke and monzogranite. Field relations, petrological,...
Zircon U–Pb dating, whole-rock major oxide, trace element and Sr–Nd–Hf isotopic data are presented for the Late Permian to Early Triassic Shijianfang batholith from Faku in North Liaoning Province, North China. Two main magmatic suites are documented: one, with an emplacement age of ca. 260Ma, is mafic to intermediate in composition, forming small gabbroic to monzonitic intrusions; the other is felsic...
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