积聚
发表于 2025-3-21 17:01:29
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乱砍
发表于 2025-3-21 22:03:08
Advanced Data Mining and Applicationsinent examples for periodites appear to be nonturbiditic pelagic to hemipelagic limestone-marl rhythms. Under favorable conditions including diagenetic enhancement of small primary alternations, they record a periodically changing environment which is otherwise obscured or obliterated.
set598
发表于 2025-3-22 03:25:34
Wenhan Dong,Shi Feng,Daling Wang,Yifei Zhangayers are composed of dark-grey limestone with an increasing dolomite content towards the margins..Metastable components of modern lime muds are aragonite, biogenous silica, and Mg-calcite. In this order they are dissolved and precipitated in the pore space of the mud forming limestone layers with the internal structure described above.
严厉谴责
发表于 2025-3-22 05:50:44
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chronology
发表于 2025-3-22 10:00:02
Rhythmic Sedimentation Documented in a Late Cretaceous Core (Abstract)d sedimentation events documented in the peels indicate that this Cretaceous sea oscillated between brackish and marine states, stratified and well-mixed states, and between anaerobic and aerobic bottom conditions.
iodides
发表于 2025-3-22 14:33:41
https://doi.org/10.1007/978-3-030-95408-6on (probably initiated by bacterial activity) within the uppermost 10 cm of sediment, and is followed by subsequent reprecipitation of the same material immediately below sea floor. The newly cemented sediment-layer remains largely unaffected during a latter phase of carbonate-solution because of its coarser grain-size.
iodides
发表于 2025-3-22 18:27:38
Diagenetic Redistribution of Carbonate, a Process in Forming Limestone-Marl Alternations (Devonian aon (probably initiated by bacterial activity) within the uppermost 10 cm of sediment, and is followed by subsequent reprecipitation of the same material immediately below sea floor. The newly cemented sediment-layer remains largely unaffected during a latter phase of carbonate-solution because of its coarser grain-size.
Evocative
发表于 2025-3-22 23:57:32
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conifer
发表于 2025-3-23 05:09:29
A Contribution to the Origin of Limestone-Shale Sequencesayers are composed of dark-grey limestone with an increasing dolomite content towards the margins..Metastable components of modern lime muds are aragonite, biogenous silica, and Mg-calcite. In this order they are dissolved and precipitated in the pore space of the mud forming limestone layers with the internal structure described above.
–吃
发表于 2025-3-23 08:31:54
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