about
Late Holocene intensification of the westerly winds at the subantarctic Auckland Islands (51° S), New ZealandThe potential influence of shallow gas and gas hydrates on sea floor erosion of Rock Garden, an uplifted ridge offshore of New ZealandComparison of fiber-optic sensor and borehole seismometer VSP surveys in a scientific borehole: DFDP-2b, Alpine Fault, New ZealandCenozoic basin evolution beneath the southern McMurdo Ice Shelf, AntarcticaA drill-hole calibrated geophysical characterisation of the 23 Ma Foulden Maar stratigraphic sequence, Otago, New ZealandHow tectonic folding influences gas hydrate formation: New Zealand’s Hikurangi subduction marginFocussed fluid flow on the Hikurangi Margin, New Zealand — Evidence from possible local upwarping of the base of gas hydrate stabilitySeismic imaging of gas conduits beneath seafloor seep sites in a shallow marine gas hydrate province, Hikurangi Margin, New ZealandLate Holocene intensification of the westerly winds at the subantarctic Auckland Islands (51° S), New ZealandA high-resolution climate record spanning the past 17 000 years recovered from Lake Ohau, South Island, New ZealandGas hydrate accumulations related to focused fluid flow in the Pegasus Basin, southern Hikurangi Margin, New ZealandSubmarine Slope Instabilities Coincident with Shallow Gas Hydrate Systems: Insights from New Zealand Examples
P50
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P50
description
academisch docent
@nl
geophysicist, researcher and associate professor
@en
name
Andrew R. Gorman
@ast
Andrew R. Gorman
@en
Andrew R. Gorman
@es
Andrew R. Gorman
@nl
type
label
Andrew R. Gorman
@ast
Andrew R. Gorman
@en
Andrew R. Gorman
@es
Andrew R. Gorman
@nl
altLabel
Andrew Gorman
@en
prefLabel
Andrew R. Gorman
@ast
Andrew R. Gorman
@en
Andrew R. Gorman
@es
Andrew R. Gorman
@nl
P106
P108
P1153
7101924415
P21
P31
P496
0000-0002-8581-0197