Moho Depth of Northern Baja California, Mexico, From Teleseismic Receiver Functions

We estimated Moho depths from data recorded by permanent and temporary broadband seismic stations deployed in northern Baja California, Mexico, using the receiver function technique. This region is composed of two subregions of contrasting geological and topographical characteristics: the Peninsular Ranges of Baja California (PRBC), a batholith with high elevations (up to 2,600 m); and the Mexicali Valley (MV) region, a sedimentary environment close to sea level. Crustal thickness derived from the P-to-S converted phases at 29 seismic stations were analyzed in three profiles: Two that cross the two subregions, in similar to W-E direction, and the third one that runs over the PRBC in a N-S direction. For the PRBC, Moho depths vary from 35 to 45 km, from 33 degrees N to 32 degrees N; and from 30 to 46 km depth from 32 degrees N to 30.5 degrees N. From a profile that crosses the subregions in the W-E direction; Moho depths vary from 45 to similar to 34 km under western and eastern PRBC, respectively; with an abrupt change of depth under the Main Gulf Escarpment (30 degrees), from similar to 32 to 30 km; and depths of 17-20 km under the MV. Moho depths of the profile in an similar to W-E direction at similar to 31.5 degrees N are from similar to 30 to 40 km, under topography that increases from 0 to 2,600 m; and became shallower (16 km depth) as the profile reaches the Gulf of California. These results show that deeper Moho is related to higher elevations with an abrupt change under the Main Gulf Escarpment, except for western PRBC where the Moho depth is not simply reflecting isostatic compensation.