...Pierre Lanari; Nicolas Riel; Stéphane Guillot; Olivier Vidal; Stéphane Schwartz; Arnaud Pêcher; Keiko H. Hattori Abstract The Stak massif, northern Pakistan, is a newly recognized occurrence of eclogite formed by the subduction of the northern margin of the Indian continent in the northwest...

...Frank C. Hawthorne; Mark A. Cooper; Neil A. Ball; Yassir A. Abdu; Petr Černý; Fernando Cámara; Brendan M. Laurs Abstract Billwiseite, ideally Sb 3+ 5 (Nb,Ta) 3 WO 18 , is an oxide mineral from a granitic pegmatite on the eastern margin of the Nanga Parbat – Haramosh massif at Stak Nala, 70 km east...

...Brendan M. Laurs; John H. Dilles; Yousaf Wairrach; Allah B. Kausar; Lawrence W. Snee Abstract Miarolitic granitic pegmatites in the Stak valley in the northeast part of the Nanga Parbat-Haramosh Massif, in northern Pakistan, locally contain economic quantities of bi- and tricolored tourmaline...

...Table 2 Neodymium isotope compositions of eclogites from the Stak massif. ...

....2015.10.022 . Lanari , P. , Riel , N. , Guillot , S. , Vidal , O. , Schwarts , S. , Pêcher , A. , and Hattori , K.H. , 2013 , Deciphering high-pressure metamorphism in collisional context using microprobe mapping methods: Application to the Stak eclogitic massif (northwest...

... ): Geological setting and petrogenesis of symmetrically zoned, miarolitic granitic pegmatites at Stak Nala, Nanga Parbat – Haramosh massif, northern Pakistan . Can. Mineral . 36 , 1 – 47 . London , D. ( 1986 ): Holmquistite as a guide to pegmatite rare metal deposits . Econ. Geol . 81 , 704...

... petrology of serpentinites sampled in the Monviso massif (Western Alps, Italy) was combined with a transmission electron microscopy study. Alpine serpentinites display a degree of serpentinization close to 100%. Antigorite is the main mineral present, forming non-pseudomorphic textures in the various...

... granitic pegmatites at Stak Nala, Nanga Parbat – Haramosh massif, northern Pakistan . Can. Mineral . 36 , 1 – 47 . London D. Morgan G.B. VI Paul K.A. Guttery B.M. ( 2012 ): Internal evolution of miarolitic granitic pegmatites at the Little Three mine, Ramona, California, U.S.A...

.... Hattori K. Desgreniers S. Rolland Y. van Melle J. Latif M. Kausar A.B. Pêcher A. ( 2008b ). – New occurrence of eclogitic continental rocks in NW Himalaya: The Stak massif in northern Pakistan . – Himal. J. Sci. , 5 , 57 – 58 . Guo L. Zhang H.F. Harris B.W...

... to the Kaghan and Stak UHP eclogites in the Nanga Parbat region ( O’Brien et al., 2001 ). The Tso Morari eclogites, lateral equivalents farther east, are also found directly adjacent to the suture zone but at the base of the HMC ( Epard and Steck, 2008 ). The Kaghan and Stak eclogites occur at the top...

... far been recorded within exhumed continental rocks. Unaltered eclogites have been reported and proved in the Kaghan Valley of northern Pakistan (Pognante and Spencer, 1991; Tonarini et a1. 1993). In addition, retrogressed eclogites have been discovered at the junction of the Stak and Indus Rivers...

... Massif region, where the river flows through narrow gorges, and/or where active thrust faults cross the river channel. This study reveals that the landslide dams appear to be one of the significant trigger factors in the formation of knickpoints along the Indus River. 1 Corresponding author email...

... using microprobe mapping methods: Application to the Stak eclogitic massif (northwest Himalaya) . Geology 41 : 111 - 114 Liou JG Ernst WG Zhang RY Tsujimori T Jahn BM ( 2009 ) Ultrahigh-pressure minerals and metamorphic terranes – The view from China . Journal...

... most notable tributaries include the Gilgit, Hunza, and Shyok and Astor Rivers, which contribute significant flows into the main stream ( Figure 1 ). Where the Indus River flows through the Skardu area in Northern Pakistan, it enters in a narrow gorge of the Nanga Perbat Haramosh Massif (NPHM) region...

.... These extensional fabrics are related more to crustal shortening and culmination of the domes by deeper level thrusting and not to any whole-scale lithospheric E–W extension. The Ama Drime massif NE of Mount Everest in south Tibet ( Fig. 5 ) shows an intermediate stage in the formation of a core complex (Jessup...