Skip to main content

Table 2 Measurements for X and Y phases

From: Dominant role of temperature on deep earthquake mechanics for the Tonga slab near the bottom of the upper mantle

   

X

   

Y

 

Event/array

h(km)

Δt (s)

Δp

Depth

A

Δt (s)

Δp

Depth

EV2/UW

677

8.6

+0.02

642

0.05

-

-

-

EV4/JA

670

7.1

+0.06

640

0.04

10.4

+0.03

627

EV6/UW

669

6.7

−0.01

642

0.07

10.2

+0.02

629

EV8/HI

673

8.0

+0.03

639

+0.10

11.6

+0.02

627

EV8/UW

673

9.6

0.00

635

0.04

-

-

-

EV9/HI

675

8.1

+0.03

641

−0.14

12.3

+0.03

624

EV10/HI

670

7.5

+0.02

639

−0.07

11.2

+0.02

624

EV11/HI

669

7.6

+0.02

638

−0.10

10.0

+0.0

628

EV13/HI

661

4.8

0.0

642

0.03

9.1

+0.02

624

  1. A is the amplitude of the X phase relative to the direct P wave. Plus or minus signs are shown for A only when the polarities are certain. HI, JA, and UW indicate Hi-net, J-array, and University of Washington array, respectively.