Geological map

Paleozoic host rocks with younger alkaline and hydrothermal mineralisation · Region VIEW

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.

REGIONAL SYNTHESIS

Geological story

The Dara-i-Pioz alkaline massif in the Alai Range is internationally significant for rare-mineral research; quartz-rich boulders and alkaline rocks host complex silicate, carbonate, and fluoride assemblages. Farther west in Sughd, the Konchoch area contains documented fluorite-bearing polymetallic deposits.

Time represented
Paleozoic host rocks with younger alkaline and hydrothermal mineralisation
Tectonic setting
Late Paleozoic collision belt where the Turkestan Ocean closed: from north to south the Turkestan–Alai flysch, the Zeravshan subduction–accretion complex and the Gissar arc, which ends at the Gissar suture
Rock record
Alkaline rocks, syenite and pegmatite, quartz-rich boulders, carbonatite-related rocks, calcite and fluorite-bearing assemblages

DOCUMENTED PROVENANCE

Linked minerals

EVIDENCE BASE

Sources for this region

Trace Elements in Calcite from the Darai Piez Alkaline MassifFaiziev & Gafurov · 2010

Documents calcite chemistry and its alkaline-massif geological setting.

The mineralogy of a unique baratovite- and miserite-bearing quartz–albite–aegirine rock from the Dara-i-Pioz Complex, northern TajikistanReguir, Chakhmouradian & Evdokimov · 1999

Documents aegirine as a principal phase and describes the metasomatically altered alkaline-rock assemblage.

Birth, life, and demise of the Andean–syn-collisional Gissar arc: Late Paleozoic tectono-magmatic-metamorphic evolution of the southwestern Tian Shan, TajikistanWorthington et al. · 2017

Divides the South Tien Shan of Tajikistan into the Gissar arc, the Zeravshan complex and the Turkestan–Alai flysch.