Heterodoxy
发表于 2025-3-23 11:42:51
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掺和
发表于 2025-3-23 13:52:04
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defile
发表于 2025-3-23 21:30:57
Porosity in Carbonates,nates more commonly display dissolution, cementation, recrystallization and grain replacement than the siliciclastic deposits. The porosity-permeability relation in carbonates may or may not be linear. Several schemes of classification of porosity of carbonates are available. Archi’s scheme (based o
GLOOM
发表于 2025-3-24 02:13:06
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许可
发表于 2025-3-24 05:47:12
Global Overpressure Scenario, the other mechanisms put forward by the authors for overpressure. This chapter reviews worldwide overpressure scenarios—from different continents, countries, (hydro-carbon bearing) rocks of different ages, structures, depths and tectonic and sedimentary regimes.
outer-ear
发表于 2025-3-24 07:38:00
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谷类
发表于 2025-3-24 11:43:50
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VOC
发表于 2025-3-24 17:42:41
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热心
发表于 2025-3-24 20:36:01
Book 2020the degree of sediments compacted after deposition. Published empirical curves- the compaction curves- are depth-wise porosity variation through which change in pore spaces from sediment surface to deeper depths e.g. up to 6 km can be delineated. Porosity is derived from well logs. Compaction curves
耐寒
发表于 2025-3-25 03:01:06
Compaction of Sediments and Different Compaction Models,ile the classical Athy’s relation on depth-wise exponential reduction of porosity is not divided into any distinct stages, the Hedberg’s model involves four stages. Weller’s model utilized Athy’s and Hedberg’s relations to deduce a sediment compaction model. Power’s compaction model additionally con