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The well position is also standardized, but only for 96- , 384-, and 1536-well plates. These are generally well followed by manufacturers: Well Positions [16] [17] 96-well plates have a 9 mm well-to-well spacing, 384-wells a 4.5 mm spacing, and 1536-wells a 2.25 mm spacing. A notable characteristic is that the well array is symmetrical when the ...
While "plate reader" usually refers to the devices described above, many variations are available. Some examples of other devices working with the microplate format are: ELISPOT plate readers, used to count the colored spots that are formed in the course of ELISPOT assays. High throughput imagers that can measure all the wells of a microplate ...
A Streetcar to Subduction and Other Plate Tectonic Trips by Public Transport in San Francisco. doi:10.1029/SP022. ISBN 0-87590-234-0. Wakabayashi, John (1992). "Nappes, Tectonics of Oblique Plate Convergence, and Metamorphic Evolution Related to 140 Million Years of Continuous Subduction, Franciscan Complex, California". The Journal of Geology.
Here, I redesigned the 96-well plate figure working from an overlay of a 96-well plate manufacturer technical drawing, and the official SLAS/ANSI 96-well plate size standards. Designed in Inkscape. 16:42, 29 May 2020: 672 × 452 (70 KB) FlowerFaerie087: Minor edit for consistent, smooth image: 15:43, 29 May 2020: 672 × 452 (76 KB) FlowerFaerie087
The Mendocino triple junction is located at the eastern end of the Mendocino fracture zone where it approaches Cape Mendocino. The Mendocino triple junction (MTJ) is the point where the Gorda plate, the North American plate, and the Pacific plate meet, in the Pacific Ocean near Cape Mendocino in northern California.
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Through a combination of uplift of the Sierran block and down-dropping of the area to the east, the Sierra rose upward. Rising far more steeply to the east than the west, the entire Sierra Nevada can be thought of as an enormous tilted fault block with a long, gentle slope westward to California's Central Valley and steep eastern slope. [2]
The fault section demarcates the boundary between the northwestward-moving Pacific plate and the eastward-moving Gorda plate. The Gorda plate is subducting beneath the North American plate just offshore of Cape Mendocino. Where the Mendocino Fault intersects the undersea trench of the subduction zone, it also meets the San Andreas Fault.