Full Professor Math. & Indus. Eng., École Polytechnique de Montréal, 06/2007–... Director GERAD research center, Montréal, 05/2015–... Associate Professor Math. & Indus. Eng., École Polytechnique de Montréal, 06/2001–05/2007 Assistant Professor Math. & Indus. Eng., École Polytechnique de Montréal, 12/2000–06/2001 Researcher Math. & Indus. Eng., École Polytechnique de Montréal, 08/1999–11/2000 A...

Full Professor Math. & Indus. Eng., École Polytechnique de Montréal, 06/2007–... Director GERAD research center, Montréal, 05/2015–... Associate Professor Math. & Indus. Eng., École Polytechnique de Montréal, 06/2001–05/2007 Assistant Professor Math. & Indus. Eng., École Polytechnique de Montréal, 12/2000–06/2001 Researcher Math. & Indus. Eng., École Polytechnique de Montréal, 08/1999–11/2000 A...

Rivers act as temporary sinks of microplastics and a key medium allowing to enter the ocean. In this study, pollution in river shore sediment Indian Himalaya, including Brahmaputra River Indus was discussed. Sampling campaigns were performed years 2018 2019. Sample pretreatment using Na 2 WO 4 ·2H O for density separation H oxidation organic material. Microplastics analysis by FTIR microscope. ...

The river tern (Sterna aurantia) is considered to be a globally vulnerable species. It native breeding resident of eastern and central Pakistan, Pan India (except the Trans-Himalayan region), Bangladesh, Myanmar, Thailand Cambodia. non-breeding in Nepal, southern Bhutan, Laos Vietnam with vagrant records from Afghanistan Iran. breeds on sandy islands freshwater lakes rivers, rarely estuaries.

Geographical Situation of Pakistan The country consists of two wings-East Pakistan and West Pakistanseparated from each other by 1,500 miles of land. By far the greater part of the population (Table I) is concentrated in the relatively small area of East Pakistan in the delta formed by the Ganges and Brahmaputra rivers, which is the most densely populated part in the world and is conspicuous fo...

Sedimentary archives in the Himalayan foreland basin and Indus submarine fan provide the most detailed records of how changing monsoon strength may have affected erosion and the development of tectonic structures in the western Himalaya during the Neogene. Muscovite Ar-Ar ages show that fast exhumation of the Greater Himalaya was earlier in the west (20–35 Ma) than in the central Himalaya (10–2...

In the third millennium B.C., the Indus Civilization flourished in northwest India and Pakistan. The late mature phase (2200-1900 B.C.) was characterized by long-distance exchange networks, planned urban settlements, sanitation facilities, standardized weights and measures, and a sphere of influence over 1,000,000 square kilometers of territory. Recent paleoclimate reconstructions from the Beas...