{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,7,11]],"date-time":"2026-07-11T01:40:29Z","timestamp":1783734029933,"version":"3.55.0"},"reference-count":25,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2000,1,1]],"date-time":"2000-01-01T00:00:00Z","timestamp":946684800000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["SP"],"published-print":{"date-parts":[[2000,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n          <jats:p>Mafic to ultramafic granulites in the northeastern part of the Jijal complex include two-pyroxene granulite, garnet-clinopyroxene granulite and garnet hornblendite. Field and textural relations indicate that two-pyroxene granulite is a relict left after formation of the garnet-clinopyroxene granulite and garnet hornblendite was an originally intrusive rock which dissected the protoliths of mafic granulites. Sm-Nd mineral isochron ages of 118 \u00b1 12 Ma, 94.0 \u00b1 4.7 Ma and 83 \u00b1 10 Ma were determined for two-pyroxene granulite, garnet-clinopyroxene granulite and garnet hornblendite respectively. These ages, together with previously reported chronological data, led to the following tectonic implications: (1) crystallization of the granulite protoliths predates, or is coeval with, the tectonic accretion of the Kohistan arc to the Asian continent; (2) crustal thickening related to the accretion was probably responsible for the high-pressure granulite-facies metamorphism in the Jijal complex; (3) formation of the garnet hornblendite assemblage was probably after crystallization of garnet-clinopyroxene granulite.<\/jats:p>","DOI":"10.1144\/gsl.sp.2000.170.01.17","type":"journal-article","created":{"date-parts":[[2008,4,30]],"date-time":"2008-04-30T18:36:18Z","timestamp":1209580578000},"page":"313-319","source":"Crossref","is-referenced-by-count":19,"title":["Timing of magmatic and metamorphic events in the Jijal complex of the Kohistan arc deduced from Sm-Nd dating of mafic granulites"],"prefix":"10.1144","volume":"170","author":[{"given":"H.","family":"Yamamoto","sequence":"first","affiliation":[{"name":"Department of Earth and Environmental Sciences, Faculty of Science, Kagoshima University\rKorimoto 1-21-35, Kagoshima 890-0065, Japan"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"E.","family":"Nakamura","sequence":"additional","affiliation":[{"name":"The Pheasant Memorial Laboratory for Geochemistry &amp; Cosmochemistry, Institute for Study of the Earth\u2019s Interior, Okayama University at Misasa\rTottori-ken 682-0193, Japan"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"1881","published-online":{"date-parts":[[2000,5,23]]},"reference":[{"key":"e_1_2_1_2_1","first-page":"345","article-title":"Chronology of subduction, collision and regional metamorphism in Kohistan, Pakistan Himalaya","volume":"9","author":"Anczkiewicz R.","year":"1997","unstructured":"Anczkiewicz R., Vance D. 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