Land Stewardship in Practice: An Example from the Eastern Pamirs of Tajikistan
2012This chapter reviews previous research and summarizes our own findings that are based on extensive fieldwork conducted between 2007 and 2010 in the Eastern Pamirs region that covers part of eastern Tajikistan, western China, and northern Afghanistan. The entry point is an overview of the post-Soviet transformation processes in Central Asia that are ...
Vanselow, Kim +2 more
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Quaternary glacial geomorphology and glaciations of Kongur Mountain, eastern Pamir, China
Science China Earth Sciences, 2011Kongur Mountain is the largest center of modern glaciation on the Pamir Plateau. During the glacial-interglacial cycles of the Quaternary, Kongur Mountain was extensively and repeatedly glaciated, and the glacial landforms from multiple glaciations are well-preserved in valleys, in basins, and on the piedmonts.
Jie Wang +4 more
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Gravity anomalies in North-Eastern Afghanistan and on the Pamirs syntaxis
Rendiconti Lincei, 1991During a survey carried out in Afghanistan in 1964 under the leadership of Prof. A. Desio, Prof. Antonio Marussi measured 64 gravity stations along profiles crossing several regions of the country. These data are published now and their meaning is explained within the context of the other gravity data available on the region including the Hindu Kush ...
Socio A. Desio, Giorgio Poretti
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MELT EVOLUTION DURING CRYSTALLIZATION OF FERGUSITE PORPHYRIES (Eastern Pamir)
Russian Geology and Geophysics, 1994Leucite fergusite porphyries from diatremes are produced during crystallization of initial parent undifferentiated magma generated under the upper mantle conditions. Study of melt inclusions in phenocrysts (leucite, apatite, clinopyroxene) has shown that phenocrysts were formed at 1300-1100 °C.
V. V. Sharygin, L. N. Pospelova
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CRANIAL CHARACTERISTICS OF THE SAKA POPULATIONS OF THE EASTERN PAMIRS
Archaeology, Ethnology and Anthropology of Eurasia, 2008This article gives an analysis of a Sakaean cranial series from the Eastern Pamirs. The predominant trait combination aligns these groups with the Eastern Mediterraneans. The crania are generally robust by Mediterranean standards; dolichocrany combines with high vault, high, narrow face.
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Branches of the Karakoram fault in Eastern Pamir
International Geology Review, 2022Wang Shifeng +4 more
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Heavy metals in aerosol samples from the Eastern Pamirs collected 2004–2006
Atmospheric Research, 2009Abstract This study measured the concentration of heavy metal elements in atmospheric aerosol samples collected between July 2004 and April 2006 at a remote site on Mt. Muztagata (38°17'N, 75°01'E, 4430 m), in the Eastern Pamirs. Inductively coupled plasma mass spectroscopy (ICP–MS) results show that the air at Muztagata contains low concentrations ...
Guangjian Wu +4 more
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A New Scandium-Bearing Variety of Tusionite from the Eastern Pamirs (Tajikistan)
Geology of Ore Deposits, 2019A new Sc-bearing variety of tusionite has been found in the Eastern Pamirs, in the near-miarolitic Dorozhny granite pegmatite complex at the Kukurt pegmatite field (left bank of the Kukurt River, 45 km east of the settlement of Murghab, Gorno-Badakhshan Autonomous Oblast, Tajikistan). Miarolitic pegmatites are related to the alpine leucocratic granites
M. A. Mirakov +4 more
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A new form of Kailasius autocrator (Lepidoptera, Papilionidae) from the eastern Pamirs
Entomological Review, 2007A new subspecies, Kailasius autocrator pshartanus, from the eastern Pamirs (the Muzkol Ridge, Sasyk River) is described. The new subspecies is distinguished from the nominative subspecies by the wing pattern and ecology. This subspecies has the most primitive wing pattern in the genus.
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Fluid inclusions in minerals and zonation of scapolite metasoms (Eastern Pamir).
2016In the article the questions of Geochemistry and Mineralogy scapolite Deposit of the East Pamirs. Scapolite mineralization is localized in metasomatity Alpine veins. Scapolite occurs in three generations. Early metamorphic scapolite. Milky-white coarse-grained scapolite. Jewelry clear crystals of scapolite from a later generation.
Rysaeva I., Rafikova F., Kubishkina E.
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