Hannu Seebeck

TL;DR: The Deep Time Model Intercomparison Project (DeepMIP) as discussed by the authors is a systematic model and data intercomparisons of three early Paleogene time slices: latest Paleocene, Paleocene-Eocene thermal maximum (PETM) and early Eocene climatic optimum (EECO).

TL;DR: In this paper, the authors examined the role of fault interactions in the development of an array of normal faults within the active Taupo Rift, New Zealand and found that these interactions are an essential feature of all fault systems on timescales of individual earthquakes to millions of years.

TL;DR: In this article, the authors used a large seismic reflection dataset, tied to wells, to document the Cretaceous-Paleocene evolution of the greater Taranaki Basin region.

TL;DR: Faulting and folding in the Southern Taranaki Basin constrain the evolution of the New Zealand plate boundary since ~−80 Â Ma as discussed by the authors, and three main phases of tectonic activity have been recognised; Late Cretaceous and Palaeocene extension, mainly Oligocene and younger contraction and Plio-Pleistocene (~ 3.7 −0 Â 0 ǫ) extension.

TL;DR: The structure and kinematics of the continental intra-arc Taupo Rift have been constrained by fault trace mapping, a large catalogue of focal mechanisms and fault slip striations.