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Polyphase Neogene basin
researchgate.net
- The Los Angeles basin is a polyphase Neogene basin within the San Andreas transform system between the Pacific and North American plates. The basin was initiated in the mid-Miocene by widespread extension associated with significant strike slip and rotation of the Transverse Ranges of southern California.
pubs.geoscienceworld.org/aapg/books/edited-volume/1338/chapter/107171168/Chapter-1-The-Los-Angeles-Basin-An-OverviewChapter 1 The Los Angeles Basin An Overview | Active Margin ...
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The Los Angeles Basin is a sedimentary basin located in Southern California, in a region known as the Peninsular Ranges. The basin is also connected to an anomalous group of east-west trending chains of mountains collectively known as the Transverse Ranges.
Jan 1, 1991 · The Los Angeles basin is a polyphase Neogene basin within the San Andreas transform system between the Pacific and North American plates. The basin was initiated in the mid-Miocene by widespread extension associated with significant strike slip and rotation of the Transverse Ranges of southern California.
The Los Angeles Basin, into which more than 80 communities of Los Angeles County are crowded, is a trough-shaped region bounded on three sides by the Santa Monica, Santa Susana, San Gabriel, San Bernadino, and Santa Ana Mountains. On its fourth side, the county looks out over the Pacific Ocean.
Written histories of the LA River typically begin when the LA basin was still an ocean, up to 10 million years ago. With seismic uplift, the ocean receded, leaving the Santa Susana, Santa Monica, and San Gabriel mountain ranges in its place. The LA River traversed the lowest passages.
Jun 29, 2016 · The Los Angeles Basin is a Miocene-age pull-apart basin that was formed by the passing of the Pacific-Juan de Fuca-North America triple junction by southern California (Nicholson et al. 1994; Ingersoll & Rumelhart 1999).
- Yiran Ma, Robert W. Clayton
- 2016
May 5, 2020 · The Los Angeles Basin is a part of the Central Groundwater Basin, shown on the figure to the right. These basins are made up of layers of aquifers and contribute to California's water supply. Due to groundwater, unstable soils and slopes can cause risk and hazard to the production of oil and gas. When saturated, minerals become corrosive and ...
About 15 million years ago, the Los Angeles Basin was underwater. As surrounding mountain ranges (including the San Gabriel and Santa Monica ranges) shifted in a clockwise spiral, the underlying crust stretched and cracked and released molten rock from below.
