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单词 detachment fault
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Examples ofdetachment fault

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The decrease of dip angles of the fault planes towards the north suggests that the faults may be connected to adetachmentfaultat depth.
From theCambridge English Corpus
If no sticking mechanism acted, shortening across the area would have been accommodated by a singledetachmentfaultwith a large movement.
From theCambridge English Corpus
This large fault therefore resembles a typical extensionaldetachmentfaultat the top of a metamorphic core complex.
From theCambridge English Corpus
In other words, thedetachmentfaultis chopped by the steeper normal faults.
From theCambridge English Corpus
This action creates a series of fault blocks, which are progressively tilted as thedetachmentfaultprogresses.
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The simple shear detachment became a deactivateddetachmentfaultonce this rifting process began the formation of new oceanic crust.
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This fault merges with a low-angledetachmentfaultat 7 km deep that developed along the top of a slightly south-dipping zone of weak salt and shale.
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It is hypothesised that this structural reorganisation is in response to evolving stress patterns associated with the development of a possibledetachmentfaultunder the volcano's west flank.
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These offshore faults could either be northwest dipping thrusts (if the overall geometry of the structure resembled a rotational slump failure) or southeast dipping (downslope-dipping) low-angle detachment faults.
From theCambridge English Corpus
This expedition was the first to associate the complex structures with detachment faults.
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However, other authors disagree that these should be called detachment faults.
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White ar rows indicate the sense of motion along low-angledetachmentfaultand the black ar rows, high-angle normal faults.
From theCambridge English Corpus
Low-angle normal faults with regional tectonic significance may be designated detachment faults.
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This effect is particularly clear in the case of detachment faults and major thrust faults.
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These deposits can grow massive because detachment faults persist for hundreds of thousands of years.
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Oblique, normal geologic fault and detachment faults in rift zones are the typical structural manifestations of transtension conditions.
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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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更新时间：2024/12/28 4:06:04