The study focuses on the major river basins within India and three transboundary basins that share boundaries with the neighboring countries such as Pakistan, Bangladesh, Bhutan, China, Nepal, Afghanistan, and Myanmar, spanning 64.5° E – 98° E and 5.5° N – 37.5° N (Fig. 1). It encompasses 15 major river basins within the Indian ...

2022年2月1日 · It is common for foreland basins to form in paleo–rift basins, whereas rift basins develop in previous compressional orogenic belts. Thus, the study of rheological variation of the lithosphere with time provides a basis for the discussion of the geodynamic evolution of a basin ( Vilotte et al., 1993 ; He and Li, 1995 ; Munteanu et al., 2013 ...

These basins were defined as “major basins” considering the size, or their hydro-political importance and each basin was uniquely associated with an MRB identifier (MRBID). Further details derived from the attribute table of MRB polygons, including basin name, continent from which the water comes, sea and ocean into which the water flows ...

2003年9月1日 · The papers in this volume are concerned with tracing the fluid history of several sedimentary basins. These papers, which were presented in a special session at the Geological Association of Canada and Mineralogical Association of Canada meeting in Calgary, Alberta, Canada in May 2000, illustrate some of the methods, techniques and approaches required to …

2025年2月1日 · Studies have found that reusable basins in health care facilities are often contaminated with bacteria. One study published in 2009 found that 98% of 92 basins grew bacteria, with the highest rates for enterococci, gram-negative bacilli, Staphylococcus aureus, and Vancomycin-resistant enterococci (VRE). 5 Another multicenter study (2011) in 88 hospitals …

Overall, the Du-MA well characterized the aridity index trajectory of individual basins, with 79.8 % of basins achieving Nash–Sutcliffe efficiency (NSE) >0.75, surpassing Greve (28.7 %) and Du (69.8 %). Additionally, the Du-MA equation also outperformed the Greve equation in evapotranspiration predictions at both the basin and grid scales.

2025年1月15日 · Karstification in these basins is significant, resulting in widespread rocky desertification. These five basins cover a total area of about 59,072 km 2. The karst development in these basins is generally consistent, with a total karst area of 49,608 km 2, accounting for 84 %. The altitude ranges from 331 to 6921 m, with exposed bedrock rates ...

2018年1月16日 · Ocean basins are formed geologically of oceanic (basalt) crust, in contrast to continental (granite) crust that forms the Earth’s major land masses. Thus some smaller “seas” that are underlain by ocean crust and are isolated from the world ocean as separate basins, such as the Mediterranean, Tasman, Coral, Caribbean, and the Red Seas, may ...

2012年12月1日 · Basins thus influence subglacial drainage system morphology and transmissivity, the thickness and distribution of basal ice and sediment layers, and the mechanisms and dynamics of ice flow. Adverse gradients that exceed 11 times that of the ice surface may even permit the formation of subglacial lakes.

2018年3月1日 · Due to wide distribution in petroleum basins, close relationship to hydrocarbon migration and accumulation and importance to drilling safety, abnormal high pressure or overpressure has long been a hot issue in petroleum geology and exploration, but the identification of overpressure formation and pressure prediction is a difficult problem.