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Volumn 47, Issue 1, 2004, Pages 123-127

Timing of the most recent surface rupture event on the ohariu fault near paraparaumu, New Zealand

Author keywords

Kawakawa Tephra; Ohariu Fault; Paleoseismology; Paraparaumu; Strike slip fault; Wellington

Indexed keywords

EARTHQUAKE RUPTURE; FAULT SLIP; GEOCHRONOLOGY; HOLOCENE;

EID: 2442716073     PISSN: 00288306     EISSN: 11758791     Source Type: Journal    
DOI: 10.1080/00288306.2004.9515041     Document Type: Article
Times cited : (13)

References (10)
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  • 3
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    • The Last Glacial Maximum in central and southern North Island, New Zealand: A paleoenvironmental reconstruction using the Kawakawa Tephra Formation as a chronostratigraphic marker
    • Pillans, B., McGlone, M., Palmer, A., Mildenhall, D., Alloway, B., and Berger, G., 1993. The Last Glacial Maximum in central and southern North Island, New Zealand:a paleoenvironmental reconstruction using the Kawakawa Tephra Formation as a chronostratigraphic marker. Palaeogeography, Palaeoclimatology, Palaeoecology, 101:283–304.
    • (1993) Palaeogeography, Palaeoclimatology, Palaeoecology , vol.101 , pp. 283-304
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    • New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.