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The method of stress inversion was first introduced by Wallace (1951) and Bott (1959) who assumed that the remote stress tensor is spatially uniform for the faulted rock and constant during the fault history, and the slip along any fault is in the same direction and sense of the maximum shear stress.
This scheme allows isolating specific faults in the closed-loop system using a purely data-based approach without requiring prior knowledge of fault history.
Non-parametric models like the artificial neural network (ANN) based models can predict software reliability based on only fault history data without any assumptions.
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The Septentrional fault's history is better known, largely because Dr. Prentice and others have done basic research on a segment in the Dominican Republic.
For example, limits and constraints might be related to the availability of datable sediments and landforms that can be used to define the recent fault kinematic history.
To explore the fault's history, a team led by Paolo Galli at the Department of Civil Protection in Rome dug trenches across it to look for soil disturbances caused by past earthquakes.
It's the fault of history, of the black hole of destruction that the Holocaust has placed in Europe and in Judaism itself, an event of quasi-Biblical incommensurability that hasn't yet found its mythopoetic representation — and that may never have one.
Of course, when wars turn out to be wars, as they always do, the enthusiasts are startled, and, with a by now familiar mixture of petulance and pomposity, shrug their shoulders and say it's all too much for anyone to understand, we're all at fault and history must take its toll.
It's the fault of history, of the black hole of destruction that the Holocaust has placed in Europe and in Judaism itself, an event of quasi-Biblical incommensurability that hasn't yet found its mythopoetic representation and that may never have one.
The large fault-parallel displacements recorded at two near-fault strong motion stations coincided with the spatiotemporal pattern of the fault slip history during the mainshock.
The large fault-parallel displacements at two near-fault stations coincided with the spatiotemporal pattern of the fault slip history during the mainshock.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com