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Crustal Architecture of the Inverted Central Lapland Rift Along the HUKKA 2007 Profile

机译:HUKKA 2007剖面上的中拉普兰中部裂谷的地壳结构

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We have studied the lateral velocity variations along a partly buried inverted paleo-rift in Central Lapland, Northern Europe with a 2D wide-angle reflection and refraction experiment, HUKKA 2007. The experiment was designed to use seven chemical explosions from commercial and military sites as sources of seismic energy. The shots were recorded by 102 stations with an average spacing of 3.45 km. Two-dimensional crustal models of variations in P-wave velocity and Vp/Vs-ratio were calculated using the ray tracing forward modeling technique. The HUKKA 2007 experiment comprises a 455 km long profile that runs NNW- SSE parallel to the Kittil? Shear Zone, a major deformation zone hosting gold deposits in the area. The profile crosses Paleoproterozoic and reactivated Archean terranes of Central Lapland. The velocity model shows a significant difference in crustal velocity structure between the northern (distances 0-120 km) and southern parts of the profile. The difference in P-wave velocities and Vp/Vs ratio can be followed through the whole crust down to the Moho boundary indicating major tectonic boundaries. Upper crustal velocities seem to vary with the terranes/compositional differences mapped at the surface. The lower layer of the upper crust displays velocities of 6.0-6.1 km/s. Both Paleoproterozoic and Archean terranes are associated with high velocity bodies (6.30-6.35 km/s) at 100 and 200-350 km distances. The Central Lapland greenstone belt and Central Lapland Granitoid complex are associated with a 4 km-thick zone of unusually low velocities (<6.0 km/s) at distances between 120 and 220 km. We interpret the HUKKA 2007 profile to image an old, partly buried, inverted continental rift zone that has been closed and modified by younger tectonic events. It has structural features typical of rifts: inward dipping rift shoulders, undulating thickness of the middle crust, high velocity lower crust and a rather uniform crustal thickness of 48 km.
机译:我们通过2D广角反射和折射实验(HUKKA 2007)研究了北欧中部拉普兰部分埋藏的倒古裂谷的横向速度变化。该实验设计为使用来自商业和军事场所的7次化学爆炸地震能量的来源。 102个电台记录了这些镜头,平均间隔为3.45公里。使用射线追踪正演建模技术计算了P波速度和Vp / Vs比率变化的二维地壳模型。 HUKKA 2007实验包括一个455公里长的剖面,该剖面与Kittil?平行运行NNW-SSE。剪切带是一个主要的变形带,在该区域拥有金矿床。剖面横跨拉普兰中部的古元古界和重新活化的太古宙山脉。速度模型显示出剖面北部(距离0-120 km)和南部之间的地壳速度结构存在显着差异。纵波速度和Vp / Vs之比的差异可以从整个地壳一直向下到Moho边界,表明主要的构造边界。上地壳速度似乎随地表处地形/成分差异而变化。上地壳的下层速度为6.0-6.1 km / s。古元古代和太古代的地层都与100和200-350 km距离处的高速体(6.30-6.35 km / s)相关。拉普兰中部绿岩带和拉普兰中部花岗岩带与一个4 km厚的异常低速带(<6.0 km / s)的区域相关,距离在120至220 km之间。我们将HUKKA 2007剖面解释为一个古老的,部分被埋藏的,倒转的大陆裂谷带,该裂谷带已被年轻的构造事件封闭和改造。它具有典型的裂谷构造特征:向内浸入裂谷肩,中地壳起伏厚度,高速下地壳和地壳厚度相当均匀的48 km。

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