ProfessorAndy Nicol

Role of faults in hydrogen generation and migration

Paleoseismology and segmentation of the Awatere Fault

Geometry and deformation of the Ostler Fault

Quantifying and Understanding Tectonic Shortening at the Hikurangi Subduction Margin, Aotearoa New Zealand

Earthquake behaviour near the Hope–Alpine fault intersection zone, Aotearoa New Zealand

Geologic mapping and fault analysis of Cretaceous and younger strata in the Monkey Face area, North Canterbury

Geometry of the Molesworth section of the Awatere Fault, Marlborough

Structural Geology and Global Geophysics

Unearthing forgotten historical earthquakes in Aotearoa New Zealand using archival records

Evolution of the Leader River in Response to Landslide Dam, Triggered by the 2016 Mw 7.8 Kaikōoura Earthquake.

New Zealand tectonic domains with a focus on the seismicity at the Southern end of the Hikurangi margin

Advanced Field Mapping

Fault Valving Mechanism in Taranaki Basin

Geometry, Displacement, and Kinematics of the Hope Fault at Mason River.

Impact of faults and fractures on seal integrity for hydrogen geostorage in Taranaki, Aotearoa, New Zealand

Basic research on the numerical model of hydrogen geo-storage

Active faulting and Hazards of the Waimea-Flaxmore Fault System, New Zealand

Using dendrochronology to accurate date earthquakes in Aotearoa New Zealand

Understanding and quantifying earthquake and tsunami hazards arising from large earthquakes on the Hikurangi-Kermadec subduction thrust

Tectonic Geomorphology of the Eastern Hope Fault and Seward Kaikoura range

Displacement and Structural Analysis of The Humps Fault along the Eastern Margin of the Culverden Basin, North Canterbury

Fault interactions and multi-fault earthquakes in the Wellington and Wairarapa regions of New Zealand

Integrating rock physics and seismic modelling for characterization of carbonates and volcanic rocks

Performance of cut and fill slopes in the 2016 Kaikōura earthquake and lessons for the resilience of infrastructure

Structure and evolution of fault zones in sedimentary rocks