ADVANCES IN FAULT SYSTEM RECOGNITION IN THE APPALACHIAN BASIN: OROGEN-PARALLEL STRIKE-SLIP TRANSPORT IN NEW YORK STATE, PENNSYLVANIA AND WEST VIRGINIA

2018 ◽  
Author(s):  
Robert D. Jacobi ◽  
◽  
Craig Eckert ◽  
Craig Eckert ◽  
Tayler Schweigel ◽  
...  
Keyword(s):  
New York ◽  
West Virginia ◽  
New York State ◽  
Appalachian Basin ◽  
Strike Slip ◽  
Fault System ◽  
York State

Source parameters of the June 13, 1967 earthquake near Lake Ontario, New York State

1977 ◽  
Vol 14 (11) ◽  
pp. 2651-2657 ◽  
Author(s):  
Michio Hashizume ◽  
Nagakoto Tange
Keyword(s):  
New York ◽  
Surface Wave ◽  
Epicentral Distance ◽  
Source Parameters ◽  
New York State ◽  
Focal Depth ◽  
Lake Ontario ◽  
Strike Slip ◽  
York State ◽  
Long Period

Source parameters of an earthquake with magnitude mb = 4.4 were determined by using surface waves. Small but clear surface wave signals were observed on long period records gathered from seismograph stations within an epicentral distance of about 2000 km. The focal mechanism was determined to be of strike-slip type with the maximum and the minimum compression axes trending NNW–SSE and ENE–WSW, respectively. The focal depth was determined to be near either 3 or 20 km.

Paleoliquefaction study of the Clarendon–Linden fault system, western New York State

2002 ◽  
Vol 353 (1-4) ◽  
pp. 263-286 ◽  
Author(s):  
Martitia P Tuttle ◽  
Kathleen Dyer-Williams ◽  
Noel L Barstow
Keyword(s):  
New York ◽  
New York State ◽  
Fault System ◽  
York State
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