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Zhang, H., Sun, M., Zhou, X. and Ying, J. (2005) Geochemical Constraints on the Origin of Mesozoic Alkaline Intrusive Complexes from the North China Craton and Tectonic Implications. Lithos, 81, 297-317.
https://doi.org/10.1016/j.lithos.2004.12.015

has been cited by the following article:

• TITLE: Gold Enrichment Patterns and Integrated Deep-Shallow Metallogenic Model of the Liaoshang Gold Deposit, Northeastern Margin of the Jiaolai Basin, China

  AUTHORS: Deping Li, Zhixin Wang, Jian Zou, Feng Hu, Junxi Yang, Jiangtao Shan

  KEYWORDS: Jiaolai Basin, Liaoshang Gold Deposit, 3D Modeling, Vertical Zonation, Metallogenic Dynamics, Exploration Targeting

  JOURNAL NAME: Open Access Library Journal, Vol.12 No.8, August 7, 2025

  ABSTRACT: The Liaoshang gold deposit in the Jiaolai Basin (North China Craton) has had its deep resource potential limited by inadequately understood vertical metallogenic patterns. Using 220 drill holes, 523 stope samples (38879.7 m), and 18,415 Au assays, this study employs implicit 3D modeling to decouple deep-shallow mineralization systems. A critical boundary at −400 m is identified: Shallow ( 5.5 g/t) are controlled by monzogranite-marble contacts, while deep (≥−400 m) stratiform orebodies (avg. 18.4 m thick, Au = 2.1 ± 0.8 g/t) follow the basin-margin detachment fault. Coefficient of variation analysis (shallow CV = 1.52 vs deep CV = 0.37) reveals a “deep pervasive alteration - shallow boiling enrichment” mechanism. Early-stage fluids formed disseminated mineralization via detachment-zone metasomatism; late-stage boiling at