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Qiao et al. (2016) commented on our work (Zhang et al., 2014) and rejected our reinterpretation of the magnetostratigraphic results of Huang et al. (2006) and Li et al. (2006), with the results gained using the Dynamic Time Warping Algorithm technique (DTWAT) as their main basis. However, Qiao et al. (2016) did not provide details of their modeling inputs, and, in particular, the parameters they chose...
The collision of India with Eurasia has caused rejuvenated deformation and uplift of the remote Tian Shan intracontinental orogenic range and has led to deposition of thick Cenozoic sediments in its flank depressions. However, our knowledge when and how the range was deformed and uplifted is still limited. We carried out detailed tectonic investigations, seismostratigraphic analysis and paleomagnetic...
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