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- Spatiotemporal differentiation and trade-offs and synergies of . . .
The basins' ecosystem services exhibits significant spatial distribution heterogeneity, generally following a “high in the center, low on the periphery” mode (Fig 3) The low value areas of ecosystem services in the three major river basins are mainly concentrated in the lower reaches of the river basins (Haikou, Chengmai, Dongfang
- Subglacial basins: Their origin and importance in glacial systems and . . .
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
- Basin Structure, Tectonics, and Stratigraphy - ScienceDirect
Oceanic sag basins form between a mid-ocean ridge by accumulating deep sea fan or basin sediments Basins also form during the subduction process related with orogenic activity Such basins are related to island arcs or an active continental margin The oceanic basins are between microcontinents and part of the continental crust
- Applicability analysis of comprehensive drought index based on GRACE . . .
In arid basins in China, the disparity between precipitation and terrestrial water storage enhances the effectiveness of the CCDI for conducting thorough drought assessments Conversely, in humid basins where changes in precipitation and terrestrial water storage occur simultaneously, the DSI is adequate for comprehensive drought evaluations
- Long-term trends in surface water quality of Chinas seven major basins . . .
The annual water flow of the seven major basins is 1 54 trillion m 3 (about 60% of the national annual water) (NBSC, 2019) Over 1 2 billion people are living in the seven basins A description of China's seven major basins and the set-up of national water quality monitoring stations is provided in Fig 1 and Supporting Information S1 (see
- Geodynamic mechanism and classification of basins in the Earth system
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
- A review on the provenance of the Voltaian Basin, Ghana: Implications . . .
Since Ghana became a petroleum-producing country, every attempt is being made to understand the sedimentary basins within the country's territorial boundaries, particularly, the Voltaian Basin This review paper investigates studies on the Voltaian Basin drawing on a comprehensive literature review based on database searches from Scopus, Web of
- Landscape fragmentation and regularity lead to . . . - ScienceDirect
The sub-basins generally followed the overall trend of the entire basin, but there were certain differences in terms of fragmentation between the Four Rivers basin and the DTLB (Fig S1) The Four Rivers showed varying degrees of increase in PD and DIVISION, with ZRB and LRB experiencing larger increases, indicating an ongoing increase in
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