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Structural Controls on Early Behavior of the 2018 Kilauea East Rift Zone Eruption Inferred from Geodetic Surveys

机译:关于2018千拓的早期行为的结构控制从大地测量推断出2011千岩东裂谷区爆发

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High-precision line-leveling on and around the Puna Geothermal Ventures (PGV) site identified structures controlling the position of dike intrusion and subsequent eruptive fissures during the onset of the 2018 eruption. Relative vertical displacements of our 32 benchmark array were measured regularly beginning in 1992. These surveys provide important background information about long-term ground motion in this part the Lower East Rift Zone (LERZ). Consistent but subtle ongoing subsidence coupled with known geologic surface features clearly defined a graben structure along the rift axis and a cross structure in the PGV area prior to the 2018 eruption. A dramatic change to the eruption of Kilauea began with the collapse and small fissure eruption at Pu‵u O‵o on April 30. For several days magma intruded into the LERZ accompanied by ground deformation and seismicity. Over the next three weeks we conducted 3 partial surveys in the area documenting unprecedented ground motion. Eruptive vents began to open on May 3, and fissures opened in a single alignment over the next nine days. Seismicity and eruptive vents were initially confined, however, to the west of PGV, impeded by a long-lived cross structure to the rift near Pohoiki Road. Relative subsidence occurred east (downrift) of this structure during this time, while uplift associated with dike intrusion presumably occurred to the west (uprift). On May 12, dike advancement across the Pohiki Road structure opened a number of new fissures south of PGV. On May 13, the only off-axis and farthest downrift eruptive vent, fissure 17, began erupting. Observed subsidence across the rift axis at PGV was abruptly replaced by significant uplift as magma broke through the cross structure and fed the eruptions downrift. Uprift migration of activity near the end of May heralded a new phase of the eruption with voluminous hotter, more fluid lavas covering most of the benchmarks used in this study.
机译:普陀地热创业(PGV)站点上和周围的高精度线路调平(PGV)站点确定了控制堤防入侵和随后的喷发裂缝在2018次喷发过程中的位置。我们的32个基准阵列的相对垂直位移是在1992年开始衡量的。这些调查在这部分下游裂口区(LERZ)中提供了关于长期地面运动的重要背景信息。与已知地质表面的一致但微妙的持续沉降在2018次喷发之前清楚地限定了沿着裂缝轴的Graben结构和PGV区域的交叉结构。对基里亚爆发的剧烈变化开始于4月30日普洱O`o的崩溃和小裂缝爆发。几天岩浆侵入了Lerz伴随着地面变形和地震性。在接下来的三周内,我们在记录前所未有的地面运动的地区进行了3个部分调查。爆发通风口开始于5月3日开放,并且在未来九天的单一方面打开裂隙。然而,地震性和喷发通风口最初被局限于PGV的西部,通过长期的交叉结构阻碍了波霍基路附近的裂缝。在此期间,这种结构的相对沉降发生(下降),而与堤防入侵相关的升起可能发生在西部(升级)。 5月12日,波西基道路结构的堤防进步开启了PGV以南的一些新裂缝。 5月13日,唯一的轴上和最远的下降爆发通风口,裂隙17开始爆发。观察到PGV的裂隙轴的沉降突然被显着的隆起所取代,因为岩浆通过交叉结构突破并射击次射击。升起活动迁移在五月末期预示着的新阶段爆发的新阶段,覆盖了本研究中使用的大部分基准的流体熔岩。

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