Options with the CMT data. Originally the Harvard CMT catalog.
The CMT method gives two focal planes, one of which is the fault plane and other the auxiliary plane. The first motions used for the CMT method do not allow a determination of which plane is which, but study of the regional geology sometimes allows that discrimination. These are FP1 and FP2, and each has a dip and strike.
Field Name | Type | Length | Explanation | Example |
EVENT_ID | string | 16 | M122604A | |
MONTH | integer | 2 | 12 | |
DAY | integer | 2 | 26 | |
YEAR | integer | 2 | 2004 | |
TIME | string | 10 | UTC | 58:50.0 |
LAT | float | 8 | Decimal degrees | 3.3 |
LONG | float | 8 | Decimal degrees | 95.78 |
DEPTH | float | 8 | km | 10 |
MB | float | 8 | Body wave magnitude mb (~Richter magnitude) | 8.9 |
MS | float | 8 | Surface wave magnitude MS (~Richter magnitude) | 8.9 |
MECH | string | 2 | Fault type (N= normal, T=thrust, S=strike slip, blank for oblique slip). Assigned by MICRODEM for color coding on maps and cross sections. | |
REGION | string | 30 | Description of the location | OFF W COAST OF NORTHERN |
FP1_STRIKE | integer | 2 | Strike in degrees of the first focal plane | 329 |
FP1_DIP | integer | 2 | Dip (from the horizontal) of the first focal plane, The dip direction is 90 degrees clockwise from the strike direction. | 8 |
FP2_STRIKE | integer | 2 | Strike of the first focal plane | 129 |
FP2_DIP | integer | 2 | Dip (from the horizontal) of the second focal plane, The dip direction is 90 degrees clockwise from the strike direction. | 83 |
PLUNGE_1 | integer | 2 | Moment tensor, first eigenvector | 52 |
STRIKE_1 | integer | 2 | 36 | |
PLUNGE_2 | integer | 2 | Moment tensor, second eigenvector | 3 |
STRIKE_2 | integer | 2 | 130 | |
PLUNGE_3 | integer | 2 | Moment tensor, third eigenvector | 38 |
STRIKE_3 | integer | 2 | 222 |
Data file will be cmt_fault_cent_MMM_YYYY.dbf, named for the last month with data:
Ekström, G., Nettles, M. & Dziewoński, A. The global CMT project 2004–2010: centroid-moment tensors for 13,017 earthquakes. Phys. Earth Planet. Inter. 200, 1–9 (2012).
Last revision 4/3/2019