• 责任者：Irshad Ahmad (University of Peshawar ; Peshawar ; Pakistan) ; Li Meijiao
• 刊名：Xinjiang Geology
• 出版年：2013
• 卷期：31(4)
• 关键词：熔结凝灰岩 ; ignimbrite ; 巴基斯坦 ; Pakistan
• 页码：p.360-370
• 图表：6 illus., 2 tables, 53 refs.
• 分类号：0801
• issnNo：ISSN1000-8845
• isbnNo：CN65-1092/P

     New isotopic ages on zircons from rocks of the Peshawar Plain Alkaline Igneous Province （PPAIP） reveal for the first time the occurrence of ignimbritic Cenozoic （Oligocene） volcanism in the Himalaya at 26.7 土 0.8 Ma.Other new ages confirm that PPAIP rift-related igneous activity was Permian and lasted From？290 Ma to ？250 Ma. Although PPAIP rocks are petrologically and geochemically typical of rifts and have been suggested to be linked to rifting on the Pangea continental margin at the initiation of the Neotethys Ocean, there are no documented rift- related structures mapped in Permian rocks of the Peshawar Plain. We suggest that Permian rift-related structures have been dismembered and/or reactivated during shortening associated with India - Asia collision. Shortening in the area between the Main Man-tle Thrust （MMT） and the Main Boundary Thrust （MBT） may be indicative of the subsurface northern extension of the Salt Range evaporites. Late Cenozoic sedimentary rocks of the Peshawar Plain deposited during and after Himalayan thrusting occupy a piggy-back basin on top of the thrust belt. Those sedimentary rocks have buried surviving evidence of Permian rift-related structures. Igneous rocks of the PPAIP have been both metamorphosed and deformed during the Hi-malayan collision and Cenozoic igneousactivity, apart from the newly recognized Gohati volcanism, has involved only the intrusion of small cross-cutting granitic bodies concentrated in areas such as Malakand that are close to the MMT. Measurements on Chingalai Gneiss zircons have confirmed the occurrence of 816 ± 70 Ma aged rocks in the Precambri-an basement of the Peshawar Plain that are comparable in age to rocks in the Malani igneous province of the Rajasthan platform ？1000 km to the south.