| no |
title |
author |
magazine |
year |
volume |
issue |
page(s) |
type |
| 1 |
A geomorphological approach to determining the Neogene to Recent tectonic deformation in the Coastal Cordillera of northern Chile (Atacama)
|
Riquelme, R
|
|
2003
|
361 |
3-4 |
p. 255-275
21 p.
|
article
|
| 2 |
contents continued
|
|
|
2003
|
361 |
3-4 |
p. VI-
1 p.
|
article
|
| 3 |
Contents Volume 361
|
|
|
2003
|
361 |
3-4 |
p. 329-330
2 p.
|
article
|
| 4 |
Deformation at Stromboli volcano (Italy) revealed by rock mechanics and structural geology
|
Tibaldi, A
|
|
2003
|
361 |
3-4 |
p. 187-204
18 p.
|
article
|
| 5 |
Deformation partitioning during folding and transposition of quartz layers
|
Lagoeiro, L
|
|
2003
|
361 |
3-4 |
p. 171-186
16 p.
|
article
|
| 6 |
Editorial Board
|
|
|
2003
|
361 |
3-4 |
p. IFC-
1 p.
|
article
|
| 7 |
How soft is the crust?
|
Ranalli, Giorgio
|
|
2003
|
361 |
3-4 |
p. 319-320
2 p.
|
article
|
| 8 |
Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China)
|
Yan, Dan-Ping
|
|
2003
|
361 |
3-4 |
p. 239-254
16 p.
|
article
|
| 9 |
Paleomagnetism of the Cretaceous Morelos and Mezcala Formations, southern Mexico
|
Molina Garza, Roberto S
|
|
2003
|
361 |
3-4 |
p. 301-317
17 p.
|
article
|
| 10 |
Reconnaissance paleomagnetism of Late Triassic blocks, Kuyul region, Northern Kamchatka Peninsula, Russia
|
Harbert, William
|
|
2003
|
361 |
3-4 |
p. 215-227
13 p.
|
article
|
| 11 |
Salt movements in the Northeast German Basin and its relation to major post-Permian tectonic phases—results from 3D structural modelling, backstripping and reflection seismic data
|
Scheck, Magdalena
|
|
2003
|
361 |
3-4 |
p. 277-299
23 p.
|
article
|
| 12 |
Strain partitioning between the Suruga Trough and the Zenisu Thrust: Neogene to present tectonic evolution in the onland and offshore Tokai district, Japan
|
Hirono, Tetsuro
|
|
2003
|
361 |
3-4 |
p. 205-214
10 p.
|
article
|
| 13 |
The Sanfandila earthquake sequence of 1998, Queretaro, Mexico: activation of an undocumented fault in the northern edge of central Trans-Mexican Volcanic Belt
|
Zúñiga, F.R.
|
|
2003
|
361 |
3-4 |
p. 229-238
10 p.
|
article
|
| 14 |
The upper crust is softer than dry quartzite
|
Burov, E.B
|
|
2003
|
361 |
3-4 |
p. 321-326
6 p.
|
article
|
| 15 |
Why is the Central Trans-Mexican Volcanic Belt (102°–99°W) in transtensive deformation? [Tectonophysics 359 (2002) 189–208]
|
Ego, Frédéric
|
|
2003
|
361 |
3-4 |
p. 327-
1 p.
|
article
|
Journal description