• Keine Ergebnisse gefunden

Fig. 3. Seismic pro

N/A
N/A
Protected

Academic year: 2022

Aktie "Fig. 3. Seismic pro"

Copied!
1
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

Fig. 3. Seismic profiles from 2004 and coring locations of surface sediments taken between 2002 and 2005. Bold lines (A–C) indicate seismic profiles shown in Figs. 8–10. The stars indicate the locations of the Saint Naum (N) and Tushemisht (T) springs, suppliers of

ground water from Lake Prespa to Lake Ohrid.

Note !

Fig. 3 was erroneously not printed in the paper;

Fig. 2 A+B was printed twice instead.

Lz1120 Lz1083

Lz1084 Lz1085 Lz1086

OHR02-1 OHR03-1

OHR03-2

00 4 km

A

B C

Referenzen

ÄHNLICHE DOKUMENTE

Far away from the source (far-field) seismic sources are best described as point-like double couple forces. The orientation of the inital displacement of P or S waves

Far away from the source (far-field) seismic sources are best described as point-like double couple forces. The orientation of the inital displacement of P or S waves

Point source characteristics (source moment tensor, rise time, source moment, rupture dimensions) give us some estimate on what happened at the fault. However we need to take a

Introduction Computational Geophysics and Data Analysis 2..

The relation between stress and strain in general is described by the tensor of elastic constants c ijkl. From the symmetry of the stress and strain tensor

Point source characteristics (source moment tensor, rise time, source moment, rupture dimensions) give us some estimate on what happened at the fault. However we need to take a

• Seismic refraction and gravity data have revealed the P wave velocity and density structure of oceanic crust along a 400 km-long profile of the crest of Suiko and Jimmu guyots

Supplementary  Figure  3  –  Migrated  multichannel  seismic  line  CA‐A.  This  line  is  shown  in  the  manuscript  in Fig.  3b.  Un‐interpreted