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Pakistan Stratigraphy
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Hispar Sar group

Karakoram-Hindukush Basin · Southern Metamorphic Belt

A marble group of the Hispar–Hunza area that hosts the celebrated Hunza rubies.

Hispar Sar group is named after the right bank of Hispar glacier and may be traced northwestward into the Hunza valley. It consists of massive marbles with aluminous schists and quartzites with dark coloured amphibolite. It has tectonic contact with Hunza granodiorite and at places this contact is intrusive. This unit hosts the famous Hunza rubies and other gemstones (Kazmi and Jan 1997, Le Fort and Pechner 2001). Earlier this unit was named as Ganesh marble by Tahirkheli (1996).

Significance. A marble-dominated group of the Karakoram metamorphic belt with a tectonic, locally intrusive contact against the Hunza Granodiorite; earlier called the Ganesh Marble (Tahirkheli, 1996). Its ruby-corundum marbles, northeast of Aliabad, formed under high-grade conditions.

Lithology
Massive marble with aluminous schist, quartzite and dark amphibolite.
Type locality
Right bank of the Hispar glacier, extending northwest into the Hunza valley
Basin
Karakoram-Hindukush Basin
Region
Southern Metamorphic Belt
Introduced by
Tahirkheli (1996)
Economic importance
Hosts the famous Hunza ruby (corundum) deposits and other gemstones.

Provinces

References

  • Malkani, M.S. & Mahmood, Z. (2017). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 24.
  • Kazmi, A.H. & Jan, M.Q. (1997). Geology and Tectonics of Pakistan. Graphic Publishers, Karachi.

Reviewer confidence: medium

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