1980
DOI: 10.3133/ofr80837
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Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan

Abstract: This program would not have been possible without the excellent support of all agencies involved, both in Pakistan and the United States. The geological information and institutional growth obtained through this program should contribute significantly toward orderly economic and scientific development in one of Asia's largest and newest nations.

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Cited by 12 publications
(26 citation statements)
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“…Our work also improved the existing geological map of the area (Calkins et al 1981). A summary of our results is provided below.…”
Section: Resultsmentioning
confidence: 72%
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“…Our work also improved the existing geological map of the area (Calkins et al 1981). A summary of our results is provided below.…”
Section: Resultsmentioning
confidence: 72%
“…We recognized a number of the rock units and named formations mapped by Calkins et al (1981), Pudsey et al (1985), and Pudsey (1986). In addition, we discovered a new mineralized zone (,20 km 2 ) using the ASTER imagery ( figure 13).…”
Section: Lithologymentioning
confidence: 98%
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“…Stauffer (1975) described Devonian in the central part of Chitral, with the Charun quartzite, Koragh dolomite and Shogram quartzite, and laterally Chitral slate. Calkins et al (1981) also gave a description of some Devonian rocks in western Chitral, with rugose corals indicating Middle to late Devonian age.…”
Section: Historic Progress Of the Discovery Of Devonian Rocks In Pakimentioning
confidence: 98%
“…1). The geology of the area is characterized by multiply deformed, variably metamorphosed, Paleozoic to Mesozoic sedimentary rocks intruded by the elongate Kafiristan, Tirich Mir, BuniZom, Kesu-Kohuzi and Garam Chasma plutons (Calkins et al, 1981;Hildebrand et al, 2000;Fig. 2).…”
Section: Background Geology and Existing Chronologymentioning
confidence: 99%