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1 Markets I: The Ecosystem and Exchange-Traded Marketsবাজার অনলাইন 2 Markets II: Rates, FX and Creditবাজার অনলাইন 3 Markets III: Commodities, Energy and Cryptoবাজার অনলাইন 4 Quantitative Methodsপদ্ধতি অনলাইন 5 Derivatives and Volatilityডেরিভেটিভস অনলাইন 6 Rates, Credit, XVA and Riskসুদহার, ঋণ ও ঝুঁকি অনলাইন 7 Research Craft: Predictors, Backtests, Measurement, Portfoliosগবেষণা অনলাইন 8 Strategies I: Equities and Futuresকৌশল অনলাইন 9 Strategies II: Volatility, Relative Value, Macro and the Bank Desksকৌশল অনলাইন 10 Microstructure and Executionএক্সিকিউশন অনলাইন 11 Market Making and High-Frequency Tradingমার্কেট মেকিং অনলাইন 12 Machine Learning for Marketsমেশিন লার্নিং অনলাইন 13 Low-Latency Softwareপ্রযুক্তি অনলাইন 14 Networks, Hardware and Trading Infrastructureপ্রযুক্তি অনলাইন 15 Research, Data and Risk Platformsপ্রযুক্তি অনলাইন 16 The Desk and the Firmপ্রতিষ্ঠান অনলাইন 17 The Industry: Firms, Roles and Careersক্যারিয়ার অনলাইন 18 Interviews I: Maths, Probability and Speedক্যারিয়ার অনলাইন 19 Interviews II: Markets, Trading Games and the Final Roundক্যারিয়ার অনলাইন 20 Interviews III: Codeক্যারিয়ার অনলাইন
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Earth and Space Sciences · পরিভাষা

Subsidence, tectonic subsidence কী?

অন্য নাম: subsidence · tectonic subsidence

Definition 23.9 University Earth and Space Sciences — Year 1 · অধ্যায় 23 — Diagenesis and Sedimentary Basins

The subsidence of a basin is the downward motion of its basement, the surface on which its sediments rest, measured relative to a fixed reference such as the centre of the Earth. Its tectonic subsidence is the part due to the processes that make the basin, as distinct from the extra sinking caused by the weight of the sediment and water that fill it; it is measured by the subsidence the basement would have had under water alone.

Four kinds of sedimentary basin in cross-section (schematic, not to scale; vertical scale exaggerated). (a) A rift: the fill thickens against the border fault of a half-graben. (b) A passive margin: a wedge of sediment thickening towards the ocean over thinned continental crust. (c) A foreland basin, deepest against the thrust belt whose weight bends it down, and fed by its debris, coarsest (conglomerate) near the belt; the belt overrides the edge of its own basin. (d) An intracratonic basin: a broad sag whose layers thicken towards the centre.
Four kinds of sedimentary basin in cross-section (schematic, not to scale; vertical scale exaggerated). (a) A rift: the fill thickens against the border fault of a half-graben. (b) A passive margin: a wedge of sediment thickening towards the ocean over thinned continental crust. (c) A foreland basin, deepest against the thrust belt whose weight bends it down, and fed by its debris, coarsest (conglomerate) near the belt; the belt overrides the edge of its own basin. (d) An intracratonic basin: a broad sag whose layers thicken towards the centre.
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