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10.1016/j.geomorph.2020.107473
Geomorphic and sedimentary evidence for the flood includes streamlined boulder-strewn bars, gravel dune fields, and terraces sloping up Fraser and lowermost Thompson valleys, opposite the present direction of current river flow.
Geomorphic and sedimentary evidence for the flood includes streamlined boulder-strewn bars, gravel dune fields, and terraces sloping up Fraser and lowermost Thompson valleys, opposite the present direction of current river flow.
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10.1016/J.EARSCIREV.2021.103738
Although the tectonic evolution of the PAO has been discussed from diverse perspectives, the spatiotemporal dynamics in the evolution of the main branch of the PAO and its relationship with the Tethys remain contentious partly because of the absence of sedimentary evidence.
Although the tectonic evolution of the PAO has been discussed from diverse perspectives, the spatiotemporal dynamics in the evolution of the main branch of the PAO and its relationship with the Tethys remain contentious partly because of the absence of sedimentary evidence.
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10.1016/j.earscirev.2021.103741
Sedimentary evidence from the upper Wuchiapingian-mid Induan Wutonggou LC indicates that the climate was generally humid-subhumid and gradually became variable toward a seasonally dry condition in early Induan.
Sedimentary evidence from the upper Wuchiapingian-mid Induan Wutonggou LC indicates that the climate was generally humid-subhumid and gradually became variable toward a seasonally dry condition in early Induan.
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10.1016/j.quascirev.2021.107052
We found sedimentary evidence of the 2015 and one previous tsunami as tabular sand sheets.
We found sedimentary evidence of the 2015 and one previous tsunami as tabular sand sheets.
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10.5194/EGUSPHERE-EGU21-531
Based on sedimentary evidence, the dynamic evolution of the rockslide in response to temperature changes were reconstructed based on frictional thermal analysis.
Based on sedimentary evidence, the dynamic evolution of the rockslide in response to temperature changes were reconstructed based on frictional thermal analysis.
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10.1130/G48940.1
3, 2 h apart), and it provides the first unmistakable sedimentary evidence for an earthquake doublet.
3, 2 h apart), and it provides the first unmistakable sedimentary evidence for an earthquake doublet.
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10.5194/EGUSPHERE-EGU21-130
</p><p>Overall, this work has provided the sedimentary evidence of modern climate change through robust observational sediment flux data over multiple decades.
</p><p>Overall, this work has provided the sedimentary evidence of modern climate change through robust observational sediment flux data over multiple decades.
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10.1007/s11442-021-1870-8
We suggest this time period can be considered as a start point for the Anthropocene based on the sedimentary evidence of closed basins, globally.
We suggest this time period can be considered as a start point for the Anthropocene based on the sedimentary evidence of closed basins, globally.
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10.5194/EGUSPHERE-EGU21-12910
Based on the sedimentary evidence and known environmental constraints at the time, we develop a glacial scenario that explains how these ice sheets, together with eustatic sea-level changes, may have affected the past oceanography of the Arctic Ocean in a fundamental way that must have led to a drastic and non-linear response to external forcing.
Based on the sedimentary evidence and known environmental constraints at the time, we develop a glacial scenario that explains how these ice sheets, together with eustatic sea-level changes, may have affected the past oceanography of the Arctic Ocean in a fundamental way that must have led to a drastic and non-linear response to external forcing.
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10.1017/S0016756820001399
Sedimentary evidence indicates that the fallout tuff was variable reworked locally, whereas the tuffaceous siltstones are interpreted as turbidites mixed with terrigenous material derived from Anatolia.
Sedimentary evidence indicates that the fallout tuff was variable reworked locally, whereas the tuffaceous siltstones are interpreted as turbidites mixed with terrigenous material derived from Anatolia.
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10.1016/j.gr.2020.08.016
Large-scale geodynamic processes not only result in magmatism, but also generate corresponding tectonic and sedimentary evidence.
Large-scale geodynamic processes not only result in magmatism, but also generate corresponding tectonic and sedimentary evidence.
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10.1525/ELEMENTA.2021.068
Our findings provide robust molecular sedimentary evidence confirming that the environmental evolution of lakes in the Yunnan–Guizhou Plateau over the past century was closely associated with enhanced anthropogenic activities.
Our findings provide robust molecular sedimentary evidence confirming that the environmental evolution of lakes in the Yunnan–Guizhou Plateau over the past century was closely associated with enhanced anthropogenic activities.
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10.1016/J.QUASCIREV.2021.106919
Well-preserved shoreline and terrace remains surrounding these lakes provide critical geomorphological and sedimentary evidence that can be used to infer past lake levels over geological timescales.
Well-preserved shoreline and terrace remains surrounding these lakes provide critical geomorphological and sedimentary evidence that can be used to infer past lake levels over geological timescales.
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10.1111/BOR.12532
However, under-estimation of run-up persisted requiring further consideration of palaeotopography and palaeo-near-shore bathymetry for it to agree with sedimentary evidence.
However, under-estimation of run-up persisted requiring further consideration of palaeotopography and palaeo-near-shore bathymetry for it to agree with sedimentary evidence.
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10.1016/J.MARGEO.2021.106574
Sedimentary evidence for enhanced volcanic eruption during the glacial/interglacial transition in the volcanically active mid-ocean ridges is still lacking.
Sedimentary evidence for enhanced volcanic eruption during the glacial/interglacial transition in the volcanically active mid-ocean ridges is still lacking.
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10.1016/J.SEDGEO.2019.01.003
This study presents detailed morphological and sedimentary evidence from six esker systems in north-central Ireland, where adjacent and interacting ice domes were characterized by changes in ice-bed thermal and hydrological properties as well as significant ice dome centre migration.
This study presents detailed morphological and sedimentary evidence from six esker systems in north-central Ireland, where adjacent and interacting ice domes were characterized by changes in ice-bed thermal and hydrological properties as well as significant ice dome centre migration.
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10.1016/J.QUASCIREV.2019.01.013
This morphosedimentary evidence is associated with MIS 5−2 sea level fluctuations.
This morphosedimentary evidence is associated with MIS 5−2 sea level fluctuations.
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10.1016/J.GEOMORPH.2019.06.023
Sedimentary evidence and morphological analysis of cross sections along the LLDL outlet channel revealed a larger, earlier lake with a total volume of 4.
Sedimentary evidence and morphological analysis of cross sections along the LLDL outlet channel revealed a larger, earlier lake with a total volume of 4.
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10.1016/J.GEOMORPH.2018.10.021
Paleofloods are flood events that occurred prior to instrumented records that are discerned from sedimentary evidence.
Paleofloods are flood events that occurred prior to instrumented records that are discerned from sedimentary evidence.
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10.1038/s41467-019-12883-2
Geochemical and sedimentary evidence suggests that these S-isotope anomalies were transferred from the paleo-continent under an oxygenated atmosphere.
Geochemical and sedimentary evidence suggests that these S-isotope anomalies were transferred from the paleo-continent under an oxygenated atmosphere.
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10.1016/J.GR.2018.11.015
The sedimentary evidences of the Mungaroo Formation show low-angle shingled progradational seismic reflection configuration.
The sedimentary evidences of the Mungaroo Formation show low-angle shingled progradational seismic reflection configuration.
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10.1016/j.sedgeo.2019.105524
Here we present sedimentary evidence (cyclone overwash deposits, beachrock boulders, and cyclone-induced clastic deposits) of historic large cyclone events from coastal dune deposits on eastern Hainan Island, China.
Here we present sedimentary evidence (cyclone overwash deposits, beachrock boulders, and cyclone-induced clastic deposits) of historic large cyclone events from coastal dune deposits on eastern Hainan Island, China.
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10.3140/bull.geosci.1726
2012), but without sedimentary evidence in the neighbourhood of the present Ougarta Range except for Hirnantian periglacial sediments.
2012), but without sedimentary evidence in the neighbourhood of the present Ougarta Range except for Hirnantian periglacial sediments.
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10.1016/J.QUASCIREV.2019.03.035
In this paper we therefore firstly present a new set of criteria for identifying the landform and sedimentary evidence that defines and characterises ice-marginal lakes.
In this paper we therefore firstly present a new set of criteria for identifying the landform and sedimentary evidence that defines and characterises ice-marginal lakes.
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10.1007/978-3-319-38864-9_6
In the third part of the chapter, an analysis of the best-documented flood-rich periods and flood peaks, namely the late 1330s–1350s, late 1390s–early 1440s and late 1470s–1520s, is presented in more detail, in combination with related documentary and sedimentary evidence.
In the third part of the chapter, an analysis of the best-documented flood-rich periods and flood peaks, namely the late 1330s–1350s, late 1390s–early 1440s and late 1470s–1520s, is presented in more detail, in combination with related documentary and sedimentary evidence.
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10.1111/1755-6724.14422
The inter-sample variability of age spectra of the Triassic samples provides sedimentary evidence for Indosinian tectonic reactivation in the Eastern Tianshan and its periphery, which could be attributed to differential exhumation of different sources driven by coeval strike-slip tectonics along deep faults.
The inter-sample variability of age spectra of the Triassic samples provides sedimentary evidence for Indosinian tectonic reactivation in the Eastern Tianshan and its periphery, which could be attributed to differential exhumation of different sources driven by coeval strike-slip tectonics along deep faults.
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10.24377/LJMU.T.00011362
This PhD research utilises, for the first time, sedimentary evidence for mid to late Quaternary environmental change in the Tequixquiac region of Central-eastern Mexico.
This PhD research utilises, for the first time, sedimentary evidence for mid to late Quaternary environmental change in the Tequixquiac region of Central-eastern Mexico.
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10.1002/esp.4542
Our knowledge of this impact can be improved by correlating long-term historical storm records with sedimentary evidence of storm surges, but so far few studies have applied such an approach.
Our knowledge of this impact can be improved by correlating long-term historical storm records with sedimentary evidence of storm surges, but so far few studies have applied such an approach.
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10.1007/978-3-319-38864-9_3
Largest in quantity, potential river flood changes, great and extraordinary floods, flood-rich periods, mainly those occurred on the Danube and partly on other rivers, are discussed, detected predominantly in archaeological and partly in sedimentary evidence.
Largest in quantity, potential river flood changes, great and extraordinary floods, flood-rich periods, mainly those occurred on the Danube and partly on other rivers, are discussed, detected predominantly in archaeological and partly in sedimentary evidence.
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10.1007/978-3-319-38864-9_1
This is followed by an overview of major medieval hydroclimatic shifts and break points detected in sedimentary evidence in different parts of Europe, with an emphasis on Central Europe,regarding lake/mire water-level changes, variability and changes in the frequency and intensity of floods captured in lake sedimentation and in river alluvia.
This is followed by an overview of major medieval hydroclimatic shifts and break points detected in sedimentary evidence in different parts of Europe, with an emphasis on Central Europe,regarding lake/mire water-level changes, variability and changes in the frequency and intensity of floods captured in lake sedimentation and in river alluvia.
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10.1177/0959683619865060
Sedimentary evidence provided by foraminifera, diatoms, testate amoebae and marine macrofossils is used to support the evidence provided by the landforms in order to assess changes in former sea levels.
Sedimentary evidence provided by foraminifera, diatoms, testate amoebae and marine macrofossils is used to support the evidence provided by the landforms in order to assess changes in former sea levels.
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Sedimentary Microfacies
Sedimentary Charcoal
Sedimentary Sequence
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Sedimentary Units
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Population Evidence
Change Evidence
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Tolerance Evidence
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Stroke Evidence
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Legal Evidence
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Variables Evidence
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