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Imaging the Deep Structure of the Central DeathValley Basin Using Receiver Function, Gravity,and Magnetic Data
Bright Spot Crustal Models Data Incorporation Death Valley Magmatic Underplating
2013/3/7
We use receiver function, gravity, and magnetic data to image the deep structures of central Death Valley. Receiver function analysis suggests the Moho is 24 km deep in the central part of the basin a...
Crustal Structure of the Salton Trough: Incorporation of Receiver Function, Gravity and Magnetic Data
Data Incorporation Crustal Models Magmatic Body Salton Trough
2013/3/7
The Salton Trough of southwestern California is inferred to be an incipient ocean basin, and is a polyphase basin with significant extension in addition to dextral shear. To further explore the origin...