@article{GhaniSobelZeilingeretal.2020,
  author    = {Ghani, Humaad and Sobel, Edward and Zeilinger, Gerold and Glodny, Johannes and Zapata, Sebastian and Irum, Irum},
  title     = {Palaeozoic and Pliocene tectonic evolution of the Salt Range constrained by low-temperature thermochronology},
  series = {Terra nova},
  volume    = {33},
  journal   = {Terra nova},
  number    = {3},
  publisher = {Wiley},
  address   = {Hoboken},
  issn      = {0954-4879},
  doi       = {10.1111/ter.12515},
  pages     = {293 -- 305},
  year      = {2020},
  abstract  = {The Salt Range in Pakistan exposes Precambrian to Pleistocene strata outcropping along the Salt Range Thrust (SRT). To better understand the in-situ Cambrian and Pliocene tectonic evolution of the Pakistan Subhimalaya, we have conducted low-temperature thermochronological analysis using apatite (U-Th-Sm)/He and fission track dating. We combine cooling ages from different samples located along the thrust front of the SRT into a thermal model that shows two major cooling events associated with rifting and regional erosion in the Late Palaeozoic and SRT activity since the Pliocene. Our results suggest that the SRT maintained a long-term average shortening rate of similar to 5-6 mm/yr and a high exhumation rate above the SRT ramp since similar to 4 Ma.},
  language  = {en}
}
@article{GhaniSobelZeilingeretal.2021,
  author    = {Ghani, Humaad and Sobel, Edward and Zeilinger, Gerold and Glodny, Johannes and Irum, Irum and Sajid, Muhammad},
  title     = {Spatio-temporal structural evolution of the Kohat fold and thrust belt of Pakistan},
  series = {Journal of structural geology},
  volume    = {145},
  journal   = {Journal of structural geology},
  publisher = {Elsevier},
  address   = {Amsterdam [u.a.]},
  issn      = {0191-8141},
  doi       = {10.1016/j.jsg.2021.104310},
  pages     = {16},
  year      = {2021},
  abstract  = {The Kohat fold and thrust belt in Pakistan shows a significantly different structural style due to the structural evolution on the double d{\´e}collement compared to the rest of the Subhimalaya. In order to better understand the spatio-temporal structural evolution of the Kohat fold and thrust belt, we combine balanced cross sections with apatite (U?Th-Sm)/He (AHe) and apatite fission track (AFT) dating. The AHe and AFT ages appear to be totally reset, allowing us to date exhumation above structural ramps. The results suggest that deformation began on the frontal Surghar thrust at-15 Ma, predating or coeval with the development of the Main Boundary thrust at-12 Ma. Deformation propagated southward from the Main Boundary thrust on double de?collements between 10 Ma and 2 Ma, resulting in a disharmonic structural style inside the Kohat fold and thrust belt. Thermal modeling of the thermochronologic data suggest that samples inside Kohat fold and thrust belt experienced cooling due to formation of the duplexes; this deformation facilitated tectonic thickening of the wedge and erosion of the Miocene to Pliocene foreland strata. The spatial distribution of AHe and AFT ages in combination with the structural forward model suggest that, in the Kohat fold and thrust belt, the wedge deformed in-sequence as a supercritical wedge (-15-12 Ma), then readjusted by out-sequence deformation (-12-0 Ma) within the Kohat fold and thrust belt into a sub-critical wedge.},
  language  = {en}
}
@misc{GhaniSobelZeilingeretal.2021,
  author    = {Ghani, Humaad and Sobel, Edward and Zeilinger, Gerold and Glodny, Johannes and Zapata, Sebastian and Irum, Irum},
  title     = {Palaeozoic and Pliocene tectonic evolution of the Salt Range constrained by low-temperature thermochronology},
  series = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  journal   = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  number    = {3},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-56256},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-562567},
  pages     = {15},
  year      = {2021},
  abstract  = {The Salt Range in Pakistan exposes Precambrian to Pleistocene strata outcropping along the Salt Range Thrust (SRT). To better understand the in-situ Cambrian and Pliocene tectonic evolution of the Pakistan Subhimalaya, we have conducted low-temperature thermochronological analysis using apatite (U-Th-Sm)/He and fission track dating. We combine cooling ages from different samples located along the thrust front of the SRT into a thermal model that shows two major cooling events associated with rifting and regional erosion in the Late Palaeozoic and SRT activity since the Pliocene. Our results suggest that the SRT maintained a long-term average shortening rate of similar to 5-6 mm/yr and a high exhumation rate above the SRT ramp since similar to 4 Ma.},
  language  = {en}
}