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all geography including DSDP/ODP Sites and Legs
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Antelope Valley (15)
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North America
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Antelope Valley
Distinguishing fault offset from climatically modulated channel deflections: Insights from the Pearblossom slip-rate site, Mojave section of the San Andreas fault, California, USA
Finite‐Source Model of the 8 July 2021 M 6.0 Antelope Valley, California, Earthquake
Real‐Time Earthquake Detection and Alerting Behavior of PLUM Ground‐Motion‐Based Early Warning in the United States
Kinematic Slip Model of the 2021 M 6.0 Antelope Valley, California, Earthquake
Paleoseismic Trenches across the Sierra Nevada and Carson Range Fronts in Antelope Valley, California, and Reno, Nevada
A major drop in seawater 87 Sr/ 86 Sr during the Middle Ordovician (Darriwilian): Links to volcanism and climate?
Reworking Diversity: Effects Of Storm Deposition On Evenness And Sampled Richness, Ordovician Of The Basin And Range, Utah And Nevada, Usa
Incorporating Parametric Uncertainty in the Design of Alternative Landfill Covers in Arid Regions
Upper Crustal Structure from the Santa Monica Mountains to the Sierra Nevada, Southern California: Tomographic Results from the Los Angeles Regional Seismic Experiment, Phase II (LARSE II)
Ground Cracks Associated with the 1994 Double Spring Flat Earthquake, West-Central Nevada
Origin of echinoderms in the Paleozoic evolutionary fauna; the role of substrates
Seismic reflection evidence for two-phase development of Tertiary basins from east-central Nevada
The Quaternary alluvial sequence of the Antelope Valley, California
Arkosic alluvium derived from the Transverse Ranges and Tehachapi Mountains and deposited in the closed basin of the Antelope Valley, California, can be subdivided into eight mappable units. The six oldest units range in age from less than 0.5 m.y. through early Holocene and form widespread fill terraces and fans that extend over several thousand km 2 of the valley floor. In contrast, the two youngest units, which consist of late Holocene and modern floodplain and channel sediments, are thin and of limited areal extent. The youngest of the six older deposits can be physically traced into nearly all drainages along both mountain ranges, which suggests nearly synchronous deposition across the region during latest Pleistocene to early Holocene time. These deposits appear to interfinger with and overlie pluvial lake deposits. The five older deposits can be recognized and correlated based on a combination of several factors such as similarity of soils, in situ shear-wave velocities, and degree of primary surface dissection. This evidence suggests that principal alluviation was regionally synchronous during the middle and late Pleistocene as well. The existence of a pervasive and uniform sequence of apparently synchronous deposits throughout the region suggests that major aggradational and degradational episodes are controlled by regional climatic fluctuations. The existence of buried soils that require long periods of time for their formation further supports a climatic control of alluviation by suggesting that principal alluvial deposition is rapid and episodic. Finally, sedimentological evidence that indicates a change in hydrologic conditions during principal alluviation and an apparent correlation among major units in the Antelope Valley to those in the eastern San Joaquin Valley strongly suggest that aggradational episodes occur during major glacial to interglacial climatic transitions.