Project Sang

TAJIKISTAN FIELD GUIDE

A continent in motion

Explore terranes, deep-crust windows, sedimentary archives, and carefully sourced mineral heritage.

Approximate positions (about ±5 km), read from the Geological and Mineral Resource Map of Tajikistan, 1:1,000,000 (V.I. Verhov, Y.A. Dyakov, N.G. Vlasov; directed by Azim Ibrohim); Snezhnoe and Abdukagor from published records (GIA Gems & Gemology, 2015; Fersman Mineralogical Museum). For learning only — not directions for collecting.

REGIONS MAP

Geological regions of Tajikistan

Tap a number to read about the region.

PAMIR123456
Geology: Macrostrat (CC BY 4.0), Generalized Geology of the World (Natural Resources Canada) · patterns: FGDC

Schematic regional map · markers show broad study areas, never mine entrances or collecting coordinates.

GEOLOGICAL REGIONS

Paleozoic arc; Cenozoic basin fill

Northern Tajikistan: Kurama

The Kurama range and the Mogoltau mountains belong to a Paleozoic volcanic arc of the Middle Tien Shan; to the south the Fergana basin buries the older rocks beneath young sediments.

Region-level geography Paleozoic host rocks with younger alkaline and hydrothermal mineralisation

South Tien Shan

The Turkestan, Zeravshan, Gissar and Alai ranges form a Late Paleozoic collision belt; its alkaline massifs and hydrothermal systems host unusually diverse minerals.

Region-level geography Cretaceous–present

Tajik Depression

A deep sedimentary archive west of the Pamir that records changing seas, rivers, subsidence, and the outward growth of the mountain belt.

Region-level geography Permian–present

North Pamir

The northern edge of the Pamir records Paleozoic–Mesozoic ocean-basin evolution and later Cenozoic uplift against the Alai and Tajik basins.

Region-level geography Paleogene–Miocene reworking of older crust

Central Pamir

A chain of metamorphic domes exposes rocks that travelled through the middle crust during collision, melting, and rapid exhumation.

Region-level geography Precambrian protoliths; Cretaceous magmatism; Cenozoic metamorphism and exhumation

South Pamir

South of the Rushan–Pshart suture: deep crystalline crust in the south-west, exposed in the giant Shakhdara–Alichur dome with the historic Kuh-i-Lal spinel district, and Permian–Jurassic sedimentary cover in the south-east.

Region-level geography Paleozoic–present

Pamir orogen

A high, actively deforming orogen where pre-Cenozoic Asian terranes were profoundly reworked during the India–Asia collision.

Region-level geography

DEEP TIME

How the Pamir became the Pamir

Asian margin assembly

Arc, ocean-basin, and accretionary systems established much of the inherited framework later incorporated into the Pamir.

Evidence

Terranes join

Final accretion of Central and South Pamir terranes assembled major parts of the pre-collision orogen.

Evidence

South Pamir magmatic pulse

A large Cretaceous batholith, including a high-flux event near 105 Ma, records subduction-related magmatism.

Evidence

Collision thickens the crust

Pamir gneiss domes record prograde burial and crustal thickening during India–Asia convergence.

Evidence

Deep crust rises

Gravitational collapse and normal-sense shear zones begin exhuming hot middle-to-lower crust in major gneiss domes.

Evidence

North Pamir uplift signal

Changes in facies, zircon provenance, and isotopes record middle–late Miocene deformation and uplift.

Evidence

An active orogen

Satellite geodesy measures uplift, shortening, and westward motion where the Pamir overrides the Tajik depression.

Evidence