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
【24h】

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圣安地列斯北部断层晚期全新世古地震的时间

获取原文
获取原文并翻译 | 示例
       

摘要

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trench沟提供了圣安德烈亚斯北部断层北海岸段晚期全新世破裂历史的数据。 1906年的地震在罗斯果园(Fort Ross Orchard)现场发生了破裂,其特征是狭窄的百叶窗山脊和相关的含新世沉积物的线性槽。横跨东北断层的断层陡峭裸露的沉积物的沟槽,被解释为是源自断层的冲积层和可能的裂缝填充沉积物,以及向上的试验性断层截断,这些断层提供了1906年之前三种可能表面破裂的证据。在1906年破裂之前发生的个别地表破裂地震之后。从冲积沉积物中收集的31种碎屑放射性碳样品的放射性碳分析限制了过去大约1000年的地震时间。根据地层排序和使用OxCal程序对放射性碳年代进行统计比较,我们估计(在置信度为95%的情况下)果园站点在1906年之前发生了3次破裂,发生在AD 1660-1812,AD 1220-1380和公元1040-1190年。附近的Fort Ross Archae营地之前的战es与这些日期一致,并进一步暗示了公元555年至950年之间发生了较早的事件。总体而言,Fort Ross Orchard和Archae营地表明1906年之前的破裂在1660-1812年,AD 1220-1380,AD 1040-1190和AD 555-950。这些破裂的时间窗与圣安地列斯断层北海岸段其他站点的结果一致。但是,还需要有关邻近断层段全新世晚期破裂事件历史的更多信息,以评估圣安德烈亚斯断层的长期行为是否涉及大的1906年型破裂和较短的,特定于段的破裂的混合。

著录项

相似文献

  • 外文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号