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B. Obo-chifeng, XMF) at the north margin of NCB show dextral strike-slip movements This kind of conjugate shearing can be variously ascribed to the NNW-SSE shortening due to i) southeastward subduction of the Mongol-Okhotsk Ocean, ii) intracontinental subduction between NCB and SCB, and iii) the collision between the Qiangtang Block and Asia in the Late Triassic. The NNW-SSE shortening also caused the eastward extrusion of the continental wedge bounded by EGF and BCF. Under this shortening-extrusion regime, local extension, represented by metamorphic core complex (MCC), and syntectonic plutons can be observed within the wedge. This complex tectonic pattern shows that this continental crust wedge did not behave as a rigid block, and the Xilamulun Fault The fault systems in the northern margin of NCB, and in Mongolia are modified from Zhang et, 2009.

. Wang, respectively. The location of sutures is modified from Webb et al. Simplified bookshelf model showing how the shortening and dextral shearing may cause a bookshelf structure with clockwise block rotation accommodated by sinistral faults and local opening of voids allowing magma emplacement, 2010.

. Li, Ar geochronological result of Xilamulun strike-slip fault. (a) Apparent 40 Ar-39 Ar age spectra of this study. Box heights and quoted errors are 2?; (b) Isochron age of this study; (c) Zircon U-Pb age of syn-strike-slip granite along Xilamulun Fualt, and muscovite 40 Ar-39 Ar age of mylonite and granitic gneiss along Xilamulun Fault, Figure 5. 40 Ar-39, 2007.

. Wang, ), respectively. The location of sutures is modified from Webb et al, 2010.