@phdthesis{Ghani2019,
  author    = {Ghani, Humaad},
  title     = {Structural evolution of the Kohat and Potwar fold and thrust belts of Pakistan},
  doi       = {10.25932/publishup-44077},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-440775},
  school      = {Universit{\"a}t Potsdam},
  pages     = {viii, 121},
  year      = {2019},
  abstract  = {Fold and thrust belts are characteristic features of collisional orogen that grow laterally through time by deforming the upper crust in response to stresses caused by convergence. The deformation propagation in the upper crust is accommodated by shortening along major folds and thrusts. The formation of these structures is influenced by the mechanical strength of d{\´e}collements, basement architecture, presence of preexisting structures and taper of the wedge. These factors control not only the sequence of deformation but also cause differences in the structural style. The Himalayan fold and thrust belt exhibits significant differences in the structural style from east to west. The external zone of the Himalayan fold and thrust belt, also called the Subhimalaya, has been extensively studied to understand the temporal development and differences in the structural style in Bhutan, Nepal and India; however, the Subhimalaya in Pakistan remains poorly studied. The Kohat and Potwar fold and thrust belts (herein called Kohat and Potwar) represent the Subhimalaya in Pakistan. The Main Boundary Thrust (MBT) marks the northern boundary of both Kohat and Potwar, showing that these belts are genetically linked to foreland-vergent deformation within the Himalayan orogen, despite the pronounced contrast in structural style. This contrast becomes more pronounced toward south, where the active strike-slip Kalabagh Fault Zone links with the Kohat and Potwar range fronts, known as the Surghar Range and the Salt Range, respectively. The Surghar and Salt Ranges developed above the Surghar Thrust (SGT) and Main Frontal Thrust (MFT). In order to understand the structural style and spatiotemporal development of the major structures in Kohat and Potwar, I have used structural modeling and low temperature thermochronolgy methods in this study. The structural modeling is based on construction of balanced cross-sections by integrating surface geology, seismic reflection profiles and well data. In order to constrain the timing and magnitude of exhumation, I used apatite (U-Th-Sm)/He (AHe) and apatite fission track (AFT) dating. The results obtained from both methods are combined to document the Paleozoic to Recent history of Kohat and Potwar. The results of this research suggest two major events in the deformation history. The first major deformation event is related to Late Paleozoic rifting associated with the development of the Neo-Tethys Ocean. The second major deformation event is related to the Late Miocene to Pliocene development of the Himalayan fold and thrust belt in the Kohat and Potwar. The Late Paleozoic rifting is deciphered by inverse thermal modelling of detrital AFT and AHe ages from the Salt Range. The process of rifting in this area created normal faulting that resulted in the exhumation/erosion of Early to Middle Paleozoic strata, forming a major unconformity between Cambrian and Permian strata that is exposed today in the Salt Range. The normal faults formed in Late Paleozoic time played an important role in localizing the Miocene-Pliocene deformation in this area. The combination of structural reconstructions and thermochronologic data suggest that deformation initiated at 15±2 Ma on the SGT ramp in the southern part of Kohat. The early movement on the SGT accreted the foreland into the Kohat deforming wedge, forming the range front. The development of the MBT at 12±2 Ma formed the northern boundary of Kohat and Potwar. Deformation propagated south of the MBT in the Kohat on double d{\´e}collements and in the Potwar on a single basal d{\´e}collement. The double d{\´e}collement in the Kohat adopted an active roof-thrust deformation style that resulted in the disharmonic structural style in the upper and lower parts of the stratigraphic section. Incremental shortening resulted in the development of duplexes in the subsurface between two d{\´e}collements and imbrication above the roof thrust. Tectonic thickening caused by duplexes resulted in cooling and exhumation above the roof thrust by removal of a thick sequence of molasse strata. The structural modelling shows that the ramps on which duplexes formed in Kohat continue as tip lines of fault propagation folds in the Potwar. The absence of a double d{\´e}collement in the Potwar resulted in the preservation of a thick sequence of molasse strata there. The temporal data suggest that deformation propagated in-sequence from ~ 8 to 3 Ma in the northern part of Kohat and Potwar; however, internal deformation in the Kohat was more intense, probably required for maintaining a critical taper after a significant load was removed above the upper d{\´e}collement. In the southern part of Potwar, a steeper basement slope (β≥3°) and the presence of salt at the base of the stratigraphic section allowed for the complete preservation of the stratigraphic wedge, showcased by very little internal deformation. Activation of the MFT at ~4 Ma allowed the Salt Range to become the range front of the Potwar. The removal of a large amount of molasse strata above the MFT ramp enhanced the role of salt in shaping the structural style of the Salt Range and Kalabagh Fault Zone. Salt accumulation and migration resulted in the formation of normal faults in both areas. Salt migration in the Kalabagh fault zone has triggered out-of-sequence movement on ramps in the Kohat. The amount of shortening calculated between the MBT and the SGT in Kohat is 75±5 km and between the MBT and the MFT in Potwar is 65±5 km. A comparable amount of shortening is accommodated in the Kohat and Potwar despite their different widths: 70 km Kohat and 150 km Potwar. In summary, this research suggests that deformation switched between different structures during the last ~15 Ma through different modes of fault propagation, resulting in different structural styles and the out-of-sequence development of Kohat and Potwar.},
  language  = {en}
}
@phdthesis{Saatchi2023,
  author    = {Saatchi, Mersa},
  title     = {Study on manufacturing of multifunctional bilayer systems},
  doi       = {10.25932/publishup-60196},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-601968},
  school      = {Universit{\"a}t Potsdam},
  pages     = {116},
  year      = {2023},
  abstract  = {Layered structures are ubiquitous in nature and industrial products, in which individual layers could have different mechanical/thermal properties and functions independently contributing to the performance of the whole layered structure for their relevant application. Tuning each layer affects the performance of the whole layered system. Pores are utilized in various disciplines, where low density, but large surfaces are demanded. Besides, open and interconnected pores would act as a transferring channel for guest chemical molecules. The shape of pores influences compression behavior of the material. Moreover, introducing pores decreases the density and subsequently the mechanical strength. To maintain defined mechanical strength under various stress, porous structure can be reinforced by adding reinforcement agent such as fiber, filler or layered structure to bear the mechanical stress on demanded application. In this context, this thesis aimed to generate new functions in bilayer systems by combining layers having different moduli and/or porosity, and to develop suitable processing techniques to access these structures. Manufacturing processes of layered structures employ often organic solvents mostly causing environmental pollution. In this regard, the studied bilayer structures here were manufactured by processes free of organic solvents. In this thesis, three bilayer systems were studied to answer the individual questions. First, while various methods of introducing pores in melt-phase are reported for one-layer constructs with simple geometry, can such methods be applied to a bilayer structure, giving two porous layers? This was addressed with Bilayer System 1. Two porous layers were obtained from melt-blending of two different polyurethanes (PU) and polyvinyl alcohol (PVA) in a co-continuous phase followed by sequential injection molding and leaching the PVA phase in deionized water. A porosity of 50 ± 5\% with a high interconnectivity was obtained, in which the pore sizes in both layers ranged from 1 µm to 100 µm with an average of 22 µm in both layers. The obtained pores were tailored by applying an annealing treatment at relevant high temperatures of 110 °C and 130 °C, which allowed the porosity to be kept constant. The disadvantage of this system is that a maximum of 50\% porosity could be reached and removal of leaching material in the weld line section of both layers is not guaranteed. Such a construct serves as a model for bilayer porous structure for determining structure-property relationships with respect to the pore size, porosity and mechanical properties of each layer. This fabrication method is also applicable to complex geometries by designing a relevant mold for injection molding. Secondly, utilizing scCO2 foaming process at elevated temperature and pressure is considered as a green manufacturing process. Employing this method as a post-treatment can alter the history orientation of polymer chains created by previous fabrication methods. Can a bilayer structure be fabricated by a combination of sequential injection molding and scCO2 foaming process, in which a porous layer is supported by a compact layer? Such a construct (Bilayer System 2) was generated by sequential injection molding of a PCL (Tm ≈ 58 °C) layer and a PLLA (Tg ≈ 58 °C) layer. Soaking this structure in the autoclave with scCO2 at T = 45 °C and P = 100 bar led to the selective foaming of PCL with a porosity of 80\%, while the PLA layer was kept compact. The scCO2 autoclave led to the formation of a porous core and skin layer of the PCL, however, the degree of crystallinity of PLLA layer increased from 0 to 50\% at the defined temperature and pressure. The microcellular structure of PCL as well as the degree of crystallinity of PLLA were controlled by increasing soaking time. Thirdly, wrinkles on surfaces in micro/nano scale alter the properties, which are surface-related. Wrinkles are formed on a surface of a bilayer structure having a compliant substrate and a stiff thin film. However, the reported wrinkles were not reversible. Moreover, dynamic wrinkles in nano and micro scale have numerous examples in nature such as gecko foot hair offering reversible adhesion and an ability of lotus leaves for self-cleaning altering hydrophobicity of the surface. It was envisioned to imitate this biomimetic function on the bilayer structure, where self-assembly on/off patterns would be realized on the surface of this construct. In summary, developing layered constructs having different properties/functions in the individual layer or exhibiting a new function as the consequence of layered structure can give novel insight for designing layered constructs in various disciplines such as packaging and transport industry, aerospace industry and health technology.},
  language  = {en}
}