Fracture Patterns Around Oyama Crater Chris Haley & Dawn Sumner, UCDavis
ENE of Oyama (ESP_017897_2045) (expect 58°)
ENE of Oyama (ESP_017897_2045)
ENE of Oyama (ESP_017897_2045)
N of Oyama (PSP_003063_2050) (expect 11°)
N of Oyama (PSP_003063_2050)
NW of Oyama (PSP_005819_2050) (expect 150°)
NW of Oyama (PSP_005819_2050)
Results to Date The dominant fracture patterns in the areas studied are not radial to Oyama crater Some areas do contain dominant fracture patterns Other areas do not show regional patterns Therefore: 1)“Local” fracturing is significant. 2) Results do not exclude fractures related to Oyama as well, maybe particularly in exposures of deeper stratigraphy