<?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>Stabilizing Effect of High Pore Fluid Pressure on Fault Growth During Drained Deformation</dc:title><dc:creator>Zega, Zachary; Zhu, Wenlu</dc:creator><dc:corporate_author/><dc:editor/><dc:description>Key Points                                                            High pore fluid pressure stabilizes fault propagation in porous sandstone deformed under drained conditions                                                  Slow faulting was associated with pervasive microcracking and diffuse shear bands only in samples deformed sufficiently slow                                                  Pervasive subcritical cracking enables slow faulting at high pore fluid pressure under drained conditions at the sample scale</dc:description><dc:publisher>Wiley</dc:publisher><dc:date>2023-08-01</dc:date><dc:nsf_par_id>10465072</dc:nsf_par_id><dc:journal_name>Journal of Geophysical Research: Solid Earth</dc:journal_name><dc:journal_volume>128</dc:journal_volume><dc:journal_issue>8</dc:journal_issue><dc:page_range_or_elocation/><dc:issn>2169-9313</dc:issn><dc:isbn/><dc:doi>https://doi.org/10.1029/2023JB026536</dc:doi><dcq:identifierAwardId>1761912; 2218314</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>