<?xml version="1.0" encoding="UTF-8"?><rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcq="http://purl.org/dc/terms/"><records count="1" morepages="false" start="1" end="1"><record rownumber="1"><dc:product_type>Journal Article</dc:product_type><dc:title>Active Deformation Constraints on the Nubia‐Somalia Plate Boundary Through Heterogenous Lithosphere of the Turkana Depression</dc:title><dc:creator>Musila, M.; Ebinger, C. J.; Bastow, I. D.; Sullivan, G.; Oliva, S. J.; Knappe, E.; Perry, M.; Kounoudis, R.; Ogden, C. S.; Bendick, R.; Mwangi, S.; Mariita, N.; Kianji, G.; Kraus, E.; Illsley‐Kemp, F.</dc:creator><dc:corporate_author/><dc:editor/><dc:description>Key Points                                                                                New 1‐D velocity model relocates 1716 earthquakes with local magnitude ranging from 1 to 4.5 and                    b                    ‐value of 1.22 ± 0.06 in Turkana Depression                                                                    Brittle strain localizes in narrow areas overlying uppermost mantle low velocity zones and avoids previously thinned crust of Mesozoic rift                                                  We redefine the modern Nubia‐Somalia plate boundary across the Turkana Depression; only a part of the 300‐km‐wide region is active</dc:description><dc:publisher/><dc:date>2023-09-01</dc:date><dc:nsf_par_id>10464105</dc:nsf_par_id><dc:journal_name>Geochemistry, Geophysics, Geosystems</dc:journal_name><dc:journal_volume>24</dc:journal_volume><dc:journal_issue>9</dc:journal_issue><dc:page_range_or_elocation/><dc:issn>1525-2027</dc:issn><dc:isbn/><dc:doi>https://doi.org/10.1029/2023GC010982</dc:doi><dcq:identifierAwardId>1824417</dcq:identifierAwardId><dc:subject/><dc:version_number/><dc:location/><dc:rights/><dc:institution/><dc:sponsoring_org>National Science Foundation</dc:sponsoring_org></record></records></rdf:RDF>