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title of the thesis - Department of Geology - Queen's University

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Figure 2.2 Structures in <strong>the</strong> Himalaya and Tibet associated with orogen-parallel extension<br />

and north-south contraction. (a) Active structures in <strong>the</strong> Himalaya, modified after Styron et<br />

al. (2011) and references <strong>the</strong>rein. Red lines represent faults associated, at least in part, with<br />

orogen-parallel extension. The Main Frontal Thrust (black) is associated with ongoing N-S<br />

contraction. Numbers in grey, and italics, refer to initiation ages <strong>of</strong> structures, and sources,<br />

respectively. (B) and (c) Simplified structural map and cross-section <strong>of</strong> <strong>the</strong> upper Karnali<br />

and surrounding regions, constructed from SRTM DEM data sheets 53_06, 53_07, and<br />

modified after Murphy and Copeland (2005), Robinson et al. (2006) and Yakymchuk and<br />

Godin (2012). Structures in black and red are associated with south-directed extrusion <strong>of</strong> <strong>the</strong><br />

GHS, and orogen-parallel extension, respectively. Abbreviations and sources: GMH – Gurla<br />

Mandhata-Humla fault, ITSZ – Indus-Tsangpo suture zone, KC – Kung Co rift,LK – Lopukangri rift, MCT - Main Central thrust, STDS - South Tibetan<br />

detachment system, TG – Thakkhola graben, TY – Tangra-Yumco rift, 1 – Phillips et al. (2004), 2 – Thiede et al. (2006), 3 – Murphy et al. (2002), 4 – Murphy<br />

and Copeland (2005), 5 – Garzione et al. (2003), 6 – Murphy et al. (2010), 7 – Kali et al. (2010), 8 – Lee et al. (2011), 9 - Williams et al. (2001), 10 – Dewane et<br />

al. (2006).<br />

17

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