COLLABORATIVE MOMA PROJECTS
Shear-Wave Splitting Beneath MOMA
Shear wave splitting measurements were taken at MOMA and other eastern North American stations to examine the continental keel and patterns of mantle flow.
[Fouch et al., 2000]
For related work, go to
Matt Fouch's Web Page.
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Anisotropy at the Base of the Mantle from SHdiff/SVdiff Waves
Differences bewteen the SHdiff and SVdiff waves observed at MOMA stations are used to examine the horizontal and vertical anisotropic variations in the D'' layer beneath the mid-Pacific.
[Fouch et al., 2001]
[Fouch et al., 2002]
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Using SPdiffKS Waves to Examine the D'' ULVZ
For related work, go to
Karen Fischer's Web Page.
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Crustal Thickness Variations Across MOMA
Receiver functions are used to examine the lateral variation of the crust across the MOMA array.
[Li et al., 2002]
For related work, go to
Aibing Li's Web Page.
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Mantle Discontinuity Depth Variations Beneath MOMA
Converted phases are used to map out the change in mantle discontinuity topography in relation to the location of the Farallon slab.
[Li et al., 1998]
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