Paleogeography of Late Eocene to earliest Miocene Te Kuiti Group, central-western North Island, New Zealand.

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Title: Paleogeography of Late Eocene to earliest Miocene Te Kuiti Group, central-western North Island, New Zealand.
Authors: Kamp, PJJ1 (AUTHOR) p.kamp@waikato.ac.nz, Tripathi, ARP1 (AUTHOR), Nelson, CS1 (AUTHOR)
Source: New Zealand Journal of Geology & Geophysics. Jun2014, Vol. 57 Issue 2, p128-148. 21p.
Subjects: Paleogeography, Geological basins, Geologic faults, Miocene Epoch, Biostratigraphy
Abstract: We present a series of 13 paleogeographic maps representing development of the Waikato–King Country Basin through the Late Eocene to Early Miocene in central-western North Island when the New Zealand platform was undergoing widespread marine inundation. The maps are the end-point of a basin analysis of the Te Kuiti Group, which has included development of a revised lithostratigraphy, biostratigraphy, chronostratigraphy and the application of facies analysis. The new stratigraphic framework has identified six major unconformity-bound sequences within the Te Kuiti Group and the paleogeographic maps are drawn for time-slices through unconformities and systems tracts. A major unconformity between the Whaingaroa Formation and the Aotea Formation dated c. 29 Ma marks the start of reverse faulting on the Taranaki Fault. At c. 27 Ma, reverse displacement on the Manganui Fault started. Several phases of displacement on the Manganui Fault ensured that land persisted over part of the Herangi High throughout the Duntroonian (Ld) and Waitakian (Lw) Stages spanning the Late Oligocene and earliest Miocene. [ABSTRACT FROM PUBLISHER]
Copyright of New Zealand Journal of Geology & Geophysics is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Label: Title
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  Data: Paleogeography of Late Eocene to earliest Miocene Te Kuiti Group, central-western North Island, New Zealand.
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  Label: Authors
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  Data: <searchLink fieldCode="AR" term="%22Kamp%2C+PJJ%22">Kamp, PJJ</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> p.kamp@waikato.ac.nz</i><br /><searchLink fieldCode="AR" term="%22Tripathi%2C+ARP%22">Tripathi, ARP</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Nelson%2C+CS%22">Nelson, CS</searchLink><relatesTo>1</relatesTo> (AUTHOR)
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  Data: <searchLink fieldCode="JN" term="%22New+Zealand+Journal+of+Geology+%26+Geophysics%22">New Zealand Journal of Geology & Geophysics</searchLink>. Jun2014, Vol. 57 Issue 2, p128-148. 21p.
– Name: Subject
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  Data: <searchLink fieldCode="DE" term="%22Paleogeography%22">Paleogeography</searchLink><br /><searchLink fieldCode="DE" term="%22Geological+basins%22">Geological basins</searchLink><br /><searchLink fieldCode="DE" term="%22Geologic+faults%22">Geologic faults</searchLink><br /><searchLink fieldCode="DE" term="%22Miocene+Epoch%22">Miocene Epoch</searchLink><br /><searchLink fieldCode="DE" term="%22Biostratigraphy%22">Biostratigraphy</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: We present a series of 13 paleogeographic maps representing development of the Waikato–King Country Basin through the Late Eocene to Early Miocene in central-western North Island when the New Zealand platform was undergoing widespread marine inundation. The maps are the end-point of a basin analysis of the Te Kuiti Group, which has included development of a revised lithostratigraphy, biostratigraphy, chronostratigraphy and the application of facies analysis. The new stratigraphic framework has identified six major unconformity-bound sequences within the Te Kuiti Group and the paleogeographic maps are drawn for time-slices through unconformities and systems tracts. A major unconformity between the Whaingaroa Formation and the Aotea Formation dated c. 29 Ma marks the start of reverse faulting on the Taranaki Fault. At c. 27 Ma, reverse displacement on the Manganui Fault started. Several phases of displacement on the Manganui Fault ensured that land persisted over part of the Herangi High throughout the Duntroonian (Ld) and Waitakian (Lw) Stages spanning the Late Oligocene and earliest Miocene. [ABSTRACT FROM PUBLISHER]
– Name: AbstractSuppliedCopyright
  Label:
  Group: Ab
  Data: <i>Copyright of New Zealand Journal of Geology & Geophysics is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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RecordInfo BibRecord:
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      – Type: doi
        Value: 10.1080/00288306.2014.904384
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      – Code: eng
        Text: English
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        PageCount: 21
        StartPage: 128
    Subjects:
      – SubjectFull: Paleogeography
        Type: general
      – SubjectFull: Geological basins
        Type: general
      – SubjectFull: Geologic faults
        Type: general
      – SubjectFull: Miocene Epoch
        Type: general
      – SubjectFull: Biostratigraphy
        Type: general
    Titles:
      – TitleFull: Paleogeography of Late Eocene to earliest Miocene Te Kuiti Group, central-western North Island, New Zealand.
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            NameFull: Kamp, PJJ
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            NameFull: Tripathi, ARP
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            NameFull: Nelson, CS
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              M: 06
              Text: Jun2014
              Type: published
              Y: 2014
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            – TitleFull: New Zealand Journal of Geology & Geophysics
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