Reasearch
(STRUCTURAL ANALYSIS OF THE EASTERN PART OF THE DARSAMAND ANTICLINE, NW HIMALAYAS PAKISTAN )
The geological mapping and structural modelling of the Darsamand Anticline leads to the following conclusions.
- The Jurassic to Paleocene age rocks are exposed on the surface in the cores of anticlines and syncline in the mapped area.
- The key structural elements of these ranges are defined by east-west trending anticlines and syncline namely Tabai Ghar Anticline, Darra Ghar Anticline and Kandao Talab Syncline that are generally asymmetrical and south verging.
- The structures in the mapped area are comprised of overturned, doubly plunging anticlines and broad synclines.
- The faults inferred in the subsurface are mostly south verging.
- The overall percentage shortening in the study area is 17.90%.
- The mapped area is dominated by east west trending regional structures and thus has undergone north-south oriented compressional stresses associated Himalayan Orogeny. 24 Core Skills
- Geological field mapping
- Rock identification and classification Stratigraphic analysis
- Structural geology interpretation
- Sample collection and documentation
- Geological reporting and data analysis
- Field safety and risk assessment Professional Experience Geoscientist (Field Work) Pakistan
- Conducted extensive fieldwork across various regions of Pakistan, studying diverse geological formations.
- Identified and analyzed sedimentary rocks, including sandstone, shale, and limestone formations.
- Investigated metamorphic rocks such as schist, marble, and gneiss, focusing on texture and mineral composition.
- Examined igneous rocks, including granite and basalt, assessing their origin and structural characteristics.
- Performed geological mapping and recorded stratigraphic data in multiple terrains.
- Collected rock and soil samples for laboratory analysis and interpretation.
- Prepared detailed field reports documenting findings and geological observations.
- Collaborated with teams to support exploration and research projects.
Study Areas
- Northern Pakistan (mountainous regions)
- Punjab (plains and salt ranges)
- Khyber Pakhtunkhwa (metamorphic terrains)
Northern Pakistan (mountainous regions) Punjab (plains and salt ranges) Khyber Pakhtunkhwa (metamorphic terrains)