Subsurface SHMAX determined from a borehole image log, onshore southern East Coast Basin, New Zealand
Author:
Affiliation:
1. Institute of Geological & Nuclear Sciences, Lower Hutt, New Zealand
Funder
Ministry of Business, Innovation and Employment
Publisher
Informa UK Limited
Subject
Earth and Planetary Sciences (miscellaneous),Geology,Geophysics
Link
https://www.tandfonline.com/doi/pdf/10.1080/00288306.2019.1570946
Reference88 articles.
1. In-situ stress directions from borehole fracture traces
2. Groundwater flow beneath Mt Taranaki, New Zealand, and implications for oil and gas migration
3. Fractures, faults, and hydrocarbon entrapment, migration and flow
4. Neogene evolution of lower trench-slope basins and wedge development in the central Hikurangi subduction margin, New Zealand
5. Evolution of the Upper Cenozoic Magmatic Arc and plate boundary in northern New Zealand
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1. Shallow Tectonic Stress Magnitudes at the Hikurangi Subduction Margin, New Zealand;Geochemistry, Geophysics, Geosystems;2023-10
2. Spatial Variation of Shallow Stress Orientation Along the Hikurangi Subduction Margin: Insights From In‐Situ Borehole Image Logging;Journal of Geophysical Research: Solid Earth;2022-05
3. A multifaceted study of the offshore Titihaoa-1 drillhole and a Neogene accretionary slope basin, Hikurangi subduction margin;New Zealand Journal of Geology and Geophysics;2021-06-10
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