Standard
Seismic wavefield modeling of lower crustal and uppermost mantle heterogeneity below the Danish Basin. / Sandrin, Alessandro; Nielsen, Lars; Thybo, Hans.
In:
Eos Trans. AGU, Fall Meet. Suppl., No. 87 (52), 2006, p. T31D-0492.
Research output: Contribution to journal › Journal article › Research
Harvard
Sandrin, A, Nielsen, L & Thybo, H 2006, 'Seismic wavefield modeling of lower crustal and uppermost mantle heterogeneity below the Danish Basin', Eos Trans. AGU, Fall Meet. Suppl., no. 87 (52), pp. T31D-0492.
APA
Sandrin, A., Nielsen, L., & Thybo, H. (2006). Seismic wavefield modeling of lower crustal and uppermost mantle heterogeneity below the Danish Basin. Eos Trans. AGU, Fall Meet. Suppl., (87 (52)), T31D-0492.
Vancouver
Sandrin A, Nielsen L, Thybo H. Seismic wavefield modeling of lower crustal and uppermost mantle heterogeneity below the Danish Basin. Eos Trans. AGU, Fall Meet. Suppl. 2006;(87 (52)):T31D-0492.
Author
Sandrin, Alessandro ; Nielsen, Lars ; Thybo, Hans. / Seismic wavefield modeling of lower crustal and uppermost mantle heterogeneity below the Danish Basin. In: Eos Trans. AGU, Fall Meet. Suppl. 2006 ; No. 87 (52). pp. T31D-0492.
Bibtex
@article{12d7e7606c3811dcbee902004c4f4f50,
title = "Seismic wavefield modeling of lower crustal and uppermost mantle heterogeneity below the Danish Basin",
abstract = "seismic methods, physics of magma bodies, reflectivity, Moho",
author = "Alessandro Sandrin and Lars Nielsen and Hans Thybo",
year = "2006",
language = "English",
pages = "T31D--0492",
journal = "Eos Trans. AGU, Fall Meet. Suppl.",
number = "87 (52)",
}
RIS
TY - JOUR
T1 - Seismic wavefield modeling of lower crustal and uppermost mantle heterogeneity below the Danish Basin
AU - Sandrin, Alessandro
AU - Nielsen, Lars
AU - Thybo, Hans
PY - 2006
Y1 - 2006
N2 - seismic methods, physics of magma bodies, reflectivity, Moho
AB - seismic methods, physics of magma bodies, reflectivity, Moho
M3 - Journal article
SP - T31D-0492
JO - Eos Trans. AGU, Fall Meet. Suppl.
JF - Eos Trans. AGU, Fall Meet. Suppl.
IS - 87 (52)
ER -
