首页> 外文期刊>Bulletin of the Seismological Society of America >Timing of Late Holocene Paleoearthquakes on the Northern San Andreas Fault at the Fort Ross Orchard Site, Sonoma County, California
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Timing of Late Holocene Paleoearthquakes on the Northern San Andreas Fault at the Fort Ross Orchard Site, Sonoma County, California

机译:加利福尼亚州索诺玛县罗斯堡果园遗址北圣安地列斯断层上晚全新世古地震的时间

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Paleoseismic trenching within Fort Ross State Historic Park provides data on the late Holocene rupture history of the North Coast segment of the northern San Andreas fault. The 1906 earthquake ruptured through the Fort Ross Orchard site, which is characterized by a narrow shutter ridge and associated linear trough containing latest Holocene sediments. Trenches across the northeast-facing fault scarp exposed sediments interpreted as scarp-derived colluvium and possible fissure-fill deposits, and tentative upward fault truncations that provide evidence of three possible surface ruptures prior to 1906. Coarse-grained scarp-derived colluvial sediments were deposited after individual surface-rupturing earthquakes that predate the 1906 rupture. Radiocarbon analyses of 31 detrital radiocarbon samples collected from the colluvial deposits constrain the timing of earthquakes over the past approximately 1000 years. Based on stratigraphic ordering and a statistical comparison of radiocarbon dates using the OxCal program, we estimate (at a 95% confidence level) that three pre-1906 surface ruptures at the Orchard site occurred at A.D. 1660–1812, A.D. 1220–1380, and A.D. 1040–1190. Previous trenches at the nearby Fort Ross Archae Camp site are consistent with these dates and further suggest the occurrence of an earlier event between A.D. 555 and 950. Collectively, the Fort Ross Orchard and Archae Camp sites suggest pre-1906 ruptures at A.D. 1660–1812, A.D. 1220–1380, A.D. 1040–1190, and A.D. 555–950. The time windows for these ruptures are consistent with results from other sites on the North Coast segment of the San Andreas fault. However, additional information on the late Holocene history of rupture events on adjacent fault segments is needed to evaluate whether the long-term behavior of the San Andreas fault involves a mix of large, 1906-type ruptures and shorter, segment-specific ruptures.
机译:罗斯堡州立历史公园 内的古地震开挖提供了有关北部圣安德烈亚斯断层北段的全新世晚期破裂历史的数据。 1906年的地震 穿过罗斯果园(Fort Ross Orchard)破裂,其特征是 狭窄的百叶窗脊和相关的线性槽,其中包含 最新的全新世沉积物。沟渠穿过东北向的 断层陡峭裸露的沉积物,这些沉积物被解释为赤道衍生的砂砾层 和可能的裂缝填充沉积物,以及暂时性的向上断层 截断提供了在1906年之前发生的三种可能的表面破裂的证据。粗粒的疤痕派生的冲积沉积物在单个表面破裂地震发生之前就沉积了下来。sups 1906年破裂。从冲积沉积物 收集的31个碎屑放射性碳样品的放射性碳分析 限制了过去大约 1000年的地震发生时间。基于地层排序和使用OxCal程序对放射性碳数据进行统计 比较,我们 估计(置信水平为95%)三个1906年以前的表面 < / sup>果园遗址的破裂发生在公元1660–1812年, AD 1220–1380和公元1040–1190。附近的Fort Ross Archae营地的先前战sup> 与这些日期一致,并且进一步暗示了公元555年至950年之间发生了更早的 事件。 。总体而言,Fort Ross 果园和Archae营地建议在1906年以前的AD 1660-1812,AD 1220-1380,AD 1040-1190, < / sup>和AD 555–950。这些破裂的时间窗 与圣安德烈亚斯断层北海岸 段其他站点的结果一致。但是,需要有关邻近断层 段的全新世晚期晚期破裂历史的附加信息 ,以评估San的长期行为 安德里亚斯断层涉及大型的1906年类型的 破裂和较短的,特定于段的破裂的混合。

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