Structure and topology of a brittle-ductile fault swarm at Crawford Knob, Franz Josef, New Zealand
نویسندگان
چکیده
We present surface and structural models of a swarm dm-scale subparallel faults exposed in ∼2000 m2 glaciated outcrop near Franz Josef Glacier, the Southern Alps New Zealand. These structures are inferred to have slipped at ∼20 km depth hanging-wall Alpine Schist Fault under conditions that were variably brittle ductile as Pacific Plate was tilted uplifted. Using field mapping, real-time kinematic GPS digital images from remotely piloted aircraft system, we created model orthophotographs ground resolution ∼1 cm map compositional layering metasediments array brittle-ductile displacing them. In order decreasing relative age (and average thickness), displaced markers schist include primary psammite pelite beds, quartz veins, deformational foliation. The been used create 2-D transects 3-D where projected down-dip, determine connectivity, topology intersection types fault swarm. Lithological variations, particularly interface between pelitic psammitic schist, control on network spacing faults.
منابع مشابه
Franz Josef Kallmann (1897?1965)
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ژورنال
عنوان ژورنال: New Zealand Journal of Geology and Geophysics
سال: 2023
ISSN: ['0028-8306', '1175-8791']
DOI: https://doi.org/10.1080/00288306.2023.2203505