GeoXpert services Pvt Ltd

GeoXpert services Pvt Ltd Welcome to GeoXpert Services — your trusted partner in Minerals and Oil & Gas Exploration.

13/07/2026

Spectacular Core of the Mughol Kot Anticlines, core by Jurassic Chilton Limestone.

A geological outcrop tells a story, but a well-prepared field sketch preserves that story long after leaving the field.D...
17/06/2026

A geological outcrop tells a story, but a well-prepared field sketch preserves that story long after leaving the field.

During geological mapping, detailed outcrop sketches are one of the most valuable tools for recording lithological contacts, structural features, alteration zones, mineralization, shears, faults, fractures, and the spatial relationship between different rock units. While photographs capture the appearance of an outcrop, sketches allow geologists to highlight critical observations and interpretations that may not be obvious in images alone.

The attached sketch was prepared in the field to document the distribution of ultramafic rocks, structural discontinuities, alteration patterns, and potential mineralized zones. Such sketches form an essential part of exploration data collection and often serve as the foundation for geological interpretation, targeting, and resource evaluation.

Good mapping is not just about observing rocks—it's about accurately recording geological information so it can be understood, analyzed, and utilized long after the fieldwork is completed.

Himalayas 💗
02/06/2026

Himalayas 💗

Different types of Geological Maps
02/06/2026

Different types of Geological Maps

East looking view of the exquisite Southern Suture, Jijal, Kohistan. The MMT brings the Kohistan Island Arc (KIA) in con...
25/05/2026

East looking view of the exquisite Southern Suture, Jijal, Kohistan. The MMT brings the Kohistan Island Arc (KIA) in contact with Indian Plate.

Main Boundary Thrust (MBT) is a regional thrust Fault, separates lesser Himalaya from outer Himalaya, it carries the pre...
25/05/2026

Main Boundary Thrust (MBT) is a regional thrust Fault, separates lesser Himalaya from outer Himalaya, it carries the pre-collision Paleozoic & Mesozoic sedimentary and meta-sedimentary rocks of the northern deformed fold and thrust belt in its hanging wall and post-collision folded Miocene foreland-basin deposits in its footwall..

Ltd is proud to announce the signing of a GIS Mapping and Geological Surveying Services Agreement with (GMC), a subs...
24/05/2026

Ltd is proud to announce the signing of a GIS Mapping and Geological Surveying Services Agreement with (GMC), a subsidiary of (PEL), for exploration activities in Shigari Bala, Skardu.

The project will involve:
• Advanced GIS Mapping
• Detailed Geological Surveying
• Drone-Based Survey & Aerial Data Acquisition
• 3D Terrain & Geological Modelling
• Data-Driven Exploration Assessment

This collaboration reflects a shared commitment toward modern, technology-driven mineral exploration and responsible mining development in Pakistan.

At GeoXpert Services, we continue to provide innovative geoscience solutions by integrating field expertise with advanced technologies to support the growth of the mining sector.

We look forward to a successful partnership with GMC & PEL and the valuable outcomes this project will bring for the future of mineral exploration in the region.

"Fig. 8. Sketch showing the deformation-metamorphism sequence of the Pyrenean Axial Zone in the Aran Valley cross-sectio...
18/05/2026

"Fig. 8. Sketch showing the deformation-metamorphism sequence of the Pyrenean Axial Zone in the Aran Valley cross-section. (A) Variscan structures D1 and subsequent first magmatic pulse and M1 metamorphism. (B) Variscan structures D2. (C) Variscan structures D3, second magmatic pulse and M2 metamorphic episode. (D) Mesozoic extension. (E) Alpine compression. AVS: Aran Valley Synclinorium, CA: Central Anticline, EVT: Eriste–Vallarties Fault, GD: Garona Dome, GT: Gavarnie Thrust, NPF: Northpyrenean Fault. (1) Maladeta Granodiorite; (2) Bossòst and Lys–Caillaouas granitoids; (3) mid and high grade metamorphism; (4) low grade metamorphism; (5) Mesozoic rocks; (6) Cambrian-Ordovician rocks; (7) Upper Ordovician rocks; (8) Silurian black shales; (9) Devonian rocks; (10) Carboniferous rocks (Culm); (11) Alpine fault; (12) Future Alpine fault; (13) Variscan fault; (14) Normal contact; (15) Unconformity; (16) SE cleavage; (17) S1 cleavage; (18) S2 cleavage; (19) S3 schistosity; (20) Isograde."

Source:
García-Sansegundo, J., Clariana, P., Rubio-Ordóñez, Á., & Soto, R. (2026). New geochronological and structural evidence of Alpine deformation overlapping existing Variscan structures (Pyrenean Axial Zone). Journal of Structural Geology, 105717.
https://doi.org/10.1016/j.jsg.2026.105717

Obastai Soka, the highest peak of the Sulaiman (>3400m), Pakistan
09/05/2026

Obastai Soka, the highest peak of the Sulaiman (>3400m), Pakistan

Address

Peshawar, Khyber Pakhtunkhwa
Peshawar
25000

Website

Alerts

Be the first to know and let us send you an email when GeoXpert services Pvt Ltd posts news and promotions. Your email address will not be used for any other purpose, and you can unsubscribe at any time.

Shortcuts

Share

Category