title: A fluid flow perspective on the diagenesis of Te Aute limestones

authors: Ricketts, Brian D.

subjects: diagenesis

abstract: Pliocene cool-water, bioclastic Te Aute limestones in East Coast Basin, New Zealand, accumulated either in shelfal shoal areas or about structurally shallow growth fold structures in the tectonically active accretionary forearc prism. Up to five stages of carbonate cementation are recognised, based on cement sequence-stratigraphic concepts, that formed on the seafloor during exposure of the limestones before burial, during burial, uplift, and deformation. Two principal fluid types are identified--topography-driven meteoric fluids and compaction-driven fluids. We have developed conceptual and quantitative models that attempt to relate the physical characteristics of fluid flow to the cement paragenesis. In particular, we have simulated the effects of uplift of the axial ranges bordering East Coast Basin in terms of the degree of penetration of a meteoric wedge into the basin. The dynamics of meteoric flow changed dramatically during uplift over the last 2 m.y. such that the modelled extent of the meteoric wedge is at least 40 km across the basin, and the penetration depth 1500 m or more corresponding with measured freshwater intersections in some oil wells. Cement-fluid relationships include: (1) true marine cements that precipitated in areas remote from shallow freshwater lenses; (2) pre-compaction cements that formed in shallow freshwater lenses beneath limestone "islands"; (3) post-compaction cements derived from compaction-driven flow during burial; (4) early uplift-related fracture-fill cements formed during deformation of the accretionary prism and uplift of the axial ranges; and (5) late uplift-related cements associated with uplift into a shallow meteoric regime.

text: A fluid flow perspective on the diagenesis of Te Aute limestones Pliocene cool-water, bioclastic Te Aute limestones in East Coast Basin, New Zealand, accumulated either in shelfal shoal areas or about structurally shallow growth fold structures in the tectonically active accretionary forearc prism. Up to five stages of carbonate cementation are recognised, based on cement sequence-stratigraphic concepts, that formed on the seafloor during exposure of the limestones before burial, during burial, uplift, and deformation. Two principal fluid types are identified--topography-driven meteoric fluids and compaction-driven fluids. We have developed conceptual and quantitative models that attempt to relate the physical characteristics of fluid flow to the cement paragenesis. In particular, we have simulated the effects of uplift of the axial ranges bordering East Coast Basin in terms of the degree of penetration of a meteoric wedge into the basin. The dynamics of meteoric flow changed dramatically during uplift over the last 2 m.y. such that the modelled extent of the meteoric wedge is at least 40 km across the basin, and the penetration depth 1500 m or more corresponding with measured freshwater intersections in some oil wells. Cement-fluid relationships include: (1) true marine cements that precipitated in areas remote from shallow freshwater lenses; (2) pre-compaction cements that formed in shallow freshwater lenses beneath limestone "islands"; (3) post-compaction cements derived from compaction-driven flow during burial; (4) early uplift-related fracture-fill cements formed during deformation of the accretionary prism and uplift of the axial ranges; and (5) late uplift-related cements associated with uplift into a shallow meteoric regime.

year: 2004-12-01

title: Co-WARe

authors: Soo, Chin-En Keith

abstract: Throughout history, humans have been creating receptacles in their daily activities to hold, keep, and preserve the rewards and objects they treasure. Applying the same notion, Co-WARe makes unique receptacles from covid data to express the information in an artistic form.

Co-WARe is an objectified presentation of all COVID-19 cases, deaths, geographically located data in each country, and the time of the data was generated. These data series project the different changes brought to each country since the beginning of COVID-19. It also provides more intuitive insight into the epidemic in all countries worldwide.

text: Co-WARe Throughout history, humans have been creating receptacles in their daily activities to hold, keep, and preserve the rewards and objects they treasure. Applying the same notion, Co-WARe makes unique receptacles from covid data to express the information in an artistic form.

Co-WARe is an objectified presentation of all COVID-19 cases, deaths, geographically located data in each country, and the time of the data was generated. These data series project the different changes brought to each country since the beginning of COVID-19. It also provides more intuitive insight into the epidemic in all countries worldwide.

year: 2022

title: Stemming the colonial environmental tide – Ecosystem-based management and shared Crown-Māori co-governance for sustaining our marine coastal estate in Aotearoa New Zealand – Summary report

authors: Joseph, Robert

subjects: Co-governance and ecosystem-based management, shared Crown-Maori governance jurisdiction over the coastal marine estate, ecosystem-based management

abstract: This summary report was prepared by Dr Robert Joseph from Te Mata Hautū Taketake – the Māori and Indigenous Governance Centre, Te Piringa Faculty of Law at the University of Waikato for the National Science Challenge Sustainable Seas Ko Ngā Moana Whakauka Project.

text: Stemming the colonial environmental tide – Ecosystem-based management and shared Crown-Māori co-governance for sustaining our marine coastal estate in Aotearoa New Zealand – Summary report This summary report was prepared by Dr Robert Joseph from Te Mata Hautū Taketake – the Māori and Indigenous Governance Centre, Te Piringa Faculty of Law at the University of Waikato for the National Science Challenge Sustainable Seas Ko Ngā Moana Whakauka Project.

year: 2023-12