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Q.-R. Meng, “What Drove Late Mesozoic Extension of the Northern China-Mongolia Tract?” Tectonophysics, Vol. 369, No. 3-4, 2003, pp. 155-174.
http://dx.doi.org/10.1016/S0040-1951(03)00195-1

has been cited by the following article:

• TITLE: Some Notes on the Lugiin Gol, Mushgai Khudag and Bayan Khoshuu Alkaline Complexes, Southern Mongolia

  AUTHORS: Munkhtsengel Baatar, Gerel Ochir, Jindrich Kynicky, Shigeru Iizumi, Piero Comin-Chiaramonti

  KEYWORDS: Mongolia; Alkaline Complexes; Carbonatites; REE Deposits

  JOURNAL NAME: International Journal of Geosciences, Vol.4 No.8, October 28, 2013

  ABSTRACT: Volcanic-plutonic alkaline complexes from Lugiin Gol, Mushgai Khudag and Bayan Khoshuu, southern Mongolia (244, 139 and 131 Ma, respectively) occur within grabens in E-W lineaments. They are represented by syenitic rock-types (silica undersaturated to slightly silica oversaturated) potassic rocks and are associated to stockworks of carbonatitic veins, dykes and so on. Geochemical characteristics and isotope systematics point to a veined mantle source particularly enriched in LILE and LREE. The carbonatitic veins show high contents of Ba, Sr, Th and REE and are suitable as potential ore deposits.