rotate2D: Rotate horizontal components of a seismic signal

View source: R/Utils.R

rotate2DR Documentation

Rotate horizontal components of a seismic signal

Description

The rotate2D() function rotates the two horizontal components of a seismic signal into Radial and Transverse components returned as a list of 2 Stream objects.

Usage

rotate2D(st1, st2, angle)

Arguments

st1

horizontal Stream from a channel set (channel name usually ending in "N", "E", "1", or "2")

st2

horizontal Stream from a channel set, complementary to st1

angle

angle (degrees) of the rotation

Details

The rotation web service returns Radial and Transverse seismic Streams, generated by rotating st1 and st2 by angle degrees.

The rotation service uses the following transformation matrix to change the output vectors for 2-D horizontal transformations

M_{2D} = ≤ft[ \begin{array}{cc} cos α & sin α \cr -sin α & cos α \end{array} \right]

≤ft[ \begin{array}{c} R \cr T \end{array} \right] = M_{2D} ≤ft[ \begin{array}{c} N \cr E \end{array} \right]

where :

   N and E represent data from the original (horizontal) orientations.
   R and T represent the Radial and Transverse components.
   \eqn{\alpha} is the azimuth angle measured clockwise from north.
  

Value

A list of two Stream objects stR and stT is returned.

Note

N and E are determined by the Stream @stats@azimuth values. If Stream @stats@azimuth values are not defined, st1 is assumed to be N and st2 is assumed to be E. Orthogonality is also assumed to be correct.

Author(s)

Jonathan Callahan jonathan@mazamascience.com

References

IRIS DMC rotation web service:

https://service.iris.edu/irisws/rotation/1/


IRISSeismic documentation built on Oct. 16, 2022, 1:09 a.m.