A joint analysis of data on the anomalous magnetic field, seismicity, and structures of the Hess deep basalts have allowed to specify propagation of the spreading zone and to correct position of the neovolcanic zone. A precise petrogeochemical analysis of various types of basalts composing the uneven-aged oceanic crust of the basin showed that magmatics of the neovolcanic zone are related to the primitive type in contrast to rift boards of differential basalts. A model of the deep structure of the Galapagos rift in the area of the western Hess Deep has been suggested.

Supplement to: Kashintsev, Georgy L; Shreider, Anatoly A (2009): Tectonics and magmatism of the Hess Deep region of the Galapagos Rift. Translated from Okeanologiya, 2009, 49(4), 559-567, Oceanology, 49(4), 515-522