Veins in Monterey Formation, CA
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Extensive networks of veins crisscross a dolomitic bed rich in organic matter within the Monterey Formation at Arroyo Burro Beach, near Santa Barbara, California. These complex interconnections of veins demonstrate the tensile stress state achieved locally due to mechanical property differences between layers within the sequence and fluid overpressure generated during diagenesis. In these otherwise relatively impermeable rock formations, intersecting fracture sets serve as vital conduits for fluid migration.
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