A5005069691- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geology and Paleoclimatology Research
- Fish Biology and Ecology Studies
- Geochemistry and Geologic Mapping
- Physiological and biochemical adaptations
- Geomagnetism and Paleomagnetism Studies
- Avian ecology and behavior
- Bone Tumor Diagnosis and Treatments
- Ocean Acidification Effects and Responses
- Insect behavior and control techniques
- Insect Utilization and Effects
- Landslides and related hazards
- Medical Imaging and Pathology Studies
- Fungal Infections and Studies
- Aquaculture disease management and microbiota
- Mineralogy and Gemology Studies
- Anomaly Detection Techniques and Applications
- Marine and fisheries research
- Bat Biology and Ecology Studies
- Insect Pest Control Strategies
- Aquaculture Nutrition and Growth
- Sarcoma Diagnosis and Treatment
- Wildlife Ecology and Conservation
Utrecht University
2020-2023
Middle East Technical University
2021
University of Haripur
2021
Aligarh Muslim University
1960-2018
Jawaharlal Nehru Medical College Hospital
2018
Apparent polar wander paths (APWPs) calculated from paleomagnetic data describe the motion of tectonic plates relative to Earth's rotation axis through geological time, providing a quantitative paleogeographic framework for studying evolution interior, surface, and atmosphere. Previous APWPs were typically collections poles, with each pole computed sites, site representing spot reading field. It was recently shown that choice how sites are distributed over poles strongly determines...
Abstract The dynamics of slab detachment and associated geological fingerprints have been inferred from various numerical analog models. These invariably use a setup with slab‐pull‐driven convergence in which detaches below mantle‐stationary trench after the arrest plate due to arrival continental lithosphere. In contrast, reconstructions show that post‐detachment is common trenches sutures are rarely during detachment. Here, we identify more realistic kinematic context using example...
Apparent polar wander paths (APWPs) calculated from paleomagnetic data describe the motion of tectonic plates relative to Earth’s rotation axis through geological time, providing a quantitative paleogeographic framework for studying evolution interior, surface, and atmosphere. Previous APWPs were typically collections poles, with each pole computed sites, site representing spot reading field. It was recently shown that choice how sites are distributed over poles strongly determines...
Ophiolites, fragments of oceanic lithosphere exposed on land, are typically found as isolated klippen in intensely deformed fold-thrust belts spanning hundreds to thousands kilometers along-strike. Ophiolites whose geochemistry indicates that they formed above subduction zones, may have been relics larger, once-coherent, tracts the leading edge an upper plate below which occurred; such were subsequently dismembered by deformation and erosion during orogenesis uplift. However, what extent...
We provide new kinematic data from the Potwar Plateau (Pakistan) to evaluate tectonic evolution of region during Neogene. The plateau is bound by two major strike-slip faults in west and east, accommodating its southwards translation.We have recognized Neogene deformation phases plateau, based on paleostress inversion Anisotropy Magnetic Susceptibility (AMS) tensors. first phase lasted until early Pliocene was characterized vertical minor stress N-S compression, implying thrust tectonics....
The dynamics of slab detachment and associated geological fingerprints have been inferred from various numerical analogue models. These invariably use a setup with slab-pull-driven convergence in which detaches below mantle-stationary trench after the arrest plate due to arrival continental lithosphere. In contrast, reconstructions show that post-detachment is common trenches sutures are rarely during detachment. Here, we identify more realistic kinematic context using example India-Asia...
A year old male presented to the orthopaedics out patients clinic with a months history of progressive pain and swelling in left shoulder without fever night sweats cough weight loss headache altered sensorium no meningeal signs He had medical diabetes chronic renal disease tuberculosis alcoholism leukaemia lymphoma AIDS Hodgkin rsquo s corticosteroid intake or any organ transplantation preoperative blood count liver function sugar levels tumor markers were all normal Serological tests...
<p> Hazara Basin is a NE-SW trending fold and thrust belt, emerged as consequence of ongoing collision between the Indian Eurasian plates. Hazara bounded by Panjal Thrust (PT) in North Main Boundary (MBT) located South. The present work deals with paleostresses outcrop fracture pattern (orientations, opening, density) different rock units exposed Ghumanwan area vicinity Abbottabad, Basin. PT MBT juxtapose various lithological along Kashmir Syntaxes (HKS). imbricate...
<p>Iran is a mosaic of continental blocks that are surrounded by Palaeo-Tethyan and Neo-Tethyan oceanic relics. Remnants the ophiolitic rock assemblages exposed around Central Iranian Microcontinent (CIM), discretely along Sanandaj-Sirjan Zone in Jaz-Murian. The Present-day “ring” distribution ophiolites not straightforwardly explained simple subduction zone architecture. One key features to solve puzzle CIM which Sabzevar north (99-77 Ma),...
Ophiolites, fragments of oceanic lithosphere exposed on land, are typically found as isolated klippen in intensely deformed fold-thrust belts spanning hundreds to thousands kilometers along-strike. Ophiolites whose geochemistry indicates that they formed above subduction zones, may have been relics larger, once-coherent, tracts the leading edge an upper plate below which occurred; such were subsequently dismembered by deformation and erosion during orogenesis uplift. However, what extent...
<p>Much of our understanding the dynamics slab break-off and its geological signatures rely on numerical models with a simplified set-up, in which follows arrival continent mantle-stationary trench, subsequent arrest plate convergence, after delay time 10 Ma or more, break off under influence pull. However, reconstructions show that tectonic reality deviates from this setup: post-collisional convergence is common, trenches are generally not stationary relative to mantle,...
<p>Iran is a mosaic of continental blocks that are surrounded by Tethyan oceanic relics. Remnants these rock assemblages exposed around the Central Iranian Microcontinent (CIM), discretely along Sanandaj-Sirjan Zone and in Jaz-Murian. The ophiolite belts surrounding CIM mainly assumed to represent narrow back-arc basins opened Cretaceous closed before Eocene. Although ophiolites as small pieces on crust today, they oceans wide enough form supra-subduction arc-related magmatic...
<p>The Eastern Iranian Orocline provides us several opportunities to study magmatism in relation tectonic events. The buckling of this orocline is accompanied by an extreme extension its Khorasan outer arc during which a calc-alkaline dike swarm, generally andesite dacite, intruded radial pattern into the Paleocene-Eocene volcano-sedimentary units, belonging platform Lut block. azimuth these dikes shows declination 30 degrees, from N300<sup>o</sup>...