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首页> 外文期刊>Sedimentary geology >Sedimentology and stratigraphy of syn-subduction Miocene fine-grained turbidites deposited in first stages of trench-slope basin development: Whakataki Formation, North Island, New Zealand
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Sedimentology and stratigraphy of syn-subduction Miocene fine-grained turbidites deposited in first stages of trench-slope basin development: Whakataki Formation, North Island, New Zealand

机译:浅谈沟槽盆地开发的第一阶段沉积物和中间粒细粒细粒浑浊浊度的沉积学与层层:Whakataki Chormation,Newshis北岛

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摘要

This study provides a detailed sedimentological, stratigraphic and depositional model for the lower Whakataki Formation. The fine-grained nature of the turbidite successions and common T-bcde successions suggests deposition associated with medial to distal submarine fan deposits. However, the textural and compositional immaturity, combined with a high carbonaceous and carbonate content of the clastic sediments indicates a proximal detrital input. In the examined section of the lower Whakataki Formation the sedimentology and facies associations identified that the turbidite successions were deposited as dilute low-density turbidity currents that transported sediment down-slope, overflowing or bypassing upper- and mid-trench-slope basins into a structurally confined lower trench-slope basin. Flows entering the structurally confined basin were deflected to the north-northeast, producing palaeo-flow along the axis of the basin and represent deposition in the early stages of trench-slope basin development. Here, we provide a depositional model for a lower (immature) trench-slope basin and highlight that the application of the 'classical' submarine-fan model to all fine-grained turbidite deposits is not always appropriate. (C) 2020 Elsevier B.V. All rights reserved.
机译:本研究为较低的Whakataki形成提供了一种详细的沉积学,地层和沉积模型。浊度连续的细粒性和常见的T-BCDE演替表明与远端潜艇风扇沉积物相关的沉积。然而,纹理和组成的不成熟,与碎屑沉积物的高碳酸盐和碳酸盐含量结合,表明了近端脱滴输入。在较低的Whakataki地层的检查部分中,沉积学和面部关联认为浊度次数沉积为稀释的低密度浊度电流,将沉积物下坡运输,溢出或绕过的上层和中间沟槽坡度成在结构上狭窄的下沟坡盆地。进入结构狭窄的盆地的流量被偏转到北 - 东北,沿盆的轴线产生古玩流,并在沟槽盆地发育的早期阶段代表沉积。在这里,我们为较低(未成熟)沟槽坡盆地提供了一种沉积模型,并突出显示“经典”潜艇模型对所有细粒浑浊沉积物的应用并不总是合适的。 (c)2020 Elsevier B.v.保留所有权利。

著录项

  • 来源
    《Sedimentary geology》 |2021年第3期|105819.1-105819.13|共13页
  • 作者单位

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia;

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia;

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia;

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia|Australian Natl Univ Res Sch Earth Sci Canberra ACT Australia;

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia;

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia;

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia;

    Geol & Nucl Sci GNS 1 Fairway Dr Avalon 5010 POB 30-368 Lower Hutt 5040 New Zealand;

    Queensland Univ Technol Sch Earth & Atmospher Sci GPO Box 2434 Brisbane Qld 4001 Australia;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sedimentology; Stratigraphy; Proximal turbidites; Trench-slope basin;

    机译:沉积物;地层;近端浊度;沟槽坡面;
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