构造活动环境中的河道-波瓣过渡带发育:对混合床发育的影响

IF 1.9 3区 地球科学 Q1 GEOLOGY Depositional Record Pub Date : 2022-02-18 DOI:10.1002/dep2.180
Hannah L. Brooks, Makoto Ito, Valentin Zuchuat, Jeff Peakall, David M. Hodgson
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引用次数: 10

摘要

航道-波瓣过渡区是位于深水航道和波瓣之间的动态区域。这里展示了一个罕见的例子,显示了日本博须半岛Kazusa弧前盆地活动边缘环境中的剥露河道-波瓣过渡带。与现有的对构造静止环境中较薄(米)矿床的年代测定较差的研究相比,该上新世-更新世露头暴露了一个具有良好年代控制的厚(数十米)槽瓣过渡带序列。这种高分辨率露头允许评估气候和相关的相对海平面变化对地层结构的作用。识别出三个发育阶段,总体呈先粗后细的上升趋势。根据与已公布数据的比较,每个阶段都被解释为记录了一个倾斜驱动的冰川海平面下降-然后上升周期。第2阶段最厚和最粗糙地层的沉积被解释为记录了一段相对海平面下降期的结束。第1和第3阶段的较薄和较细地层形成于间冰期,在间冰期,更强的黑潮洋流,加上季风驱动的热带气旋频率和强度的增加,可能导致下坡沉积物转移受到抑制。在这种情况下,通道-波瓣过渡带沉积物的一个关键方面是存在各种各样的混合床,而之前的工作主要与波瓣边缘有关。在这里,混合床特征和粒度变化用于评估纵向和垂直偏析过程的相对重要性,并与现有模型进行比较。与构造静止盆地填充物中的槽-叶过渡带相比,该槽-叶转换带显示出较少的旁通流证据(即较厚的地层、更孤立的冲刷填充物、更少的旁通滞后),并且具有明显更多的混合床。这些特征可能在活动盆地-河道-凸角过渡带中很常见,原因是:高沉降率;高沉降率;以及构造活动斜坡的不平衡。这种不平衡可能使易受侵蚀的富泥基底恢复活力,导致富泥流到达河道-波瓣过渡带,并迅速减速,形成混合床。
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Channel-lobe transition zone development in tectonically active settings: Implications for hybrid bed development

Channel-lobe transition zones are dynamic areas located between deepwater channels and lobes. Presented here is a rare example of an exhumed channel-lobe transition zone from an active-margin setting, in the Kazusa forearc Basin, Boso Peninsula, Japan. This Plio-Pleistocene outcrop exposes a thick (tens of metres) channel-lobe transition zone succession with excellent dating control, in contrast to existing poorly dated studies of thinner (metres) deposits in tectonically quiescent settings. This high-resolution outcrop permits the roles of climate and associated relative sea-level changes on stratigraphic architecture to be assessed. Three development stages are recognised with an overall coarsening-upward then fining-upwards trend. Each stage is interpreted to record one obliquity-driven glacioeustatic sea-level fall-then-rise cycle, based on comparison with published data. Deposition of the thickest and coarsest strata, Stage 2, is interpreted to record the end of a period of relative sea-level fall. The thinner and finer strata of Stages 1 and 3 formed during interglacial periods where the stronger Kuroshio Oceanic Current, coupled to increased monsoonally driven tropical cyclone frequency and intensity, likely resulted in inhibited downslope sediment transfer. A key aspect of channel-lobe transition zone deposits in this case is the presence of a diverse range of hybrid beds, in contrast to previous work where they have primarily been associated with lobe fringes. Here hybrid bed characteristics, and grain-size variations, are used to assess the relative importance of longitudinal and vertical segregation processes, and compared to existing models. Compared to channel-lobe transition zones in tectonically quiescent basin-fills, this channel-lobe transition zone shows less evidence of bypassing flows (i.e. thicker stratigraphy, more isolated scour-fills, fewer bypass lags) and has significantly more hybrid beds. These features may be common in active basin channel-lobe transition zones due to: high subsidence rates; high sedimentation rates; and disequilibrium of tectonically active slopes. This disequilibrium could rejuvenate erodible mud-rich substrate, leading to mud-rich flows arriving at the channel-lobe transition zone, and decelerating rapidly, forming hybrid beds.

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来源期刊
CiteScore
4.10
自引率
16.70%
发文量
42
审稿时长
16 weeks
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Issue Information Issue Information The early–middle Cambrian siliciclastic tide-dominated succession in eastern Korea Preservation of groove mark striae formed by armoured mud clasts: The role of armour sediment size and bed yield stress Micritisation products in the inner ramp settings of the Abu Dhabi Lagoon
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