首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Physical properties of ultrahigh-pressure metamorphic rocks from the Sulu terrain, eastern central China: implications for the seismic structure at the Donghai (CCSD) drilling site
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Physical properties of ultrahigh-pressure metamorphic rocks from the Sulu terrain, eastern central China: implications for the seismic structure at the Donghai (CCSD) drilling site

机译:中国中部东部苏鲁地区超高压变质岩的物理性质:对东海(CCSD)钻探现场地震结构的影响

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About 30 samples representing major lithologies of Sulu ultrahigh-pressure (UHP) metamorphic rocks were collected from surface exposures and exploration wells, and compressional (Vp) and shear wave (Vs) velocities and their directional dependence (anisotropy) were determined over a range of constant confining pressures up to 600 MPa and temperatures ranging from 20 to 600 degreesC. Samples range in composition from acidic to ultramafic. P- and S-wave velocities measured at 600 MPa vary from 5.08 to 8.64 km/s and 2.34 to 4.93 km/s, respectively. Densities are in the range from 2.60 to 3.68 g/cm(3). To make a direct tie between seismic measurements (refraction and reflection) and subsurface lithologies, the experimental velocity data (corresponding to shallow depths) were used to calculate velocity profiles for the different lithologies and profiles of reflection coefficients at possible lithologic interfaces across the projected 5000-m Chinese Continental Scientific Drilling Program (CCSD) crustal segment. Comparison of calculated in situ velocities with respective intrinsic velocities suggests that the in situ velocities at shallow depths are lowered by an increased abundance of open microcracks. The strongly reflective zone beneath the Donghai drill site can be explained by the impedance contrasts between the different lithologies. Contacts between eclogite/peridotite and felsic rocks (gt-gneiss, granitic gneiss), in particular, may give rise to strong seismic reflections. In addition, shear-induced (lattice preferred orientation (LPO)-related) seismic anisotropy can increase reflectivity. For the explanation of the high velocity bodies (>6.4 km/s) around 1000 m and below 3200-m depth, large proportions of eclogite/peridotite (about 40 and 30 vol.%, respectively) are needed. (C) 2002 Elsevier Science B.V. All rights reserved. [References: 37]
机译:从地表暴露和勘探井中收集了大约30个代表苏鲁超高压(UHP)变质岩主要岩性的样品,并确定了在恒定的围压高达600 MPa,温度范围从20到600摄氏度。样品的组成范围从酸性到超镁铁质。在600 MPa下测得的P波和S波速度分别从5.08至8.64 km / s和2.34至4.93 km / s变化。密度范围是2.60至3.68 g / cm(3)。为了在地震测量(折射和反射)与地下岩性之间建立直接联系,使用了实验速度数据(对应于浅层深度)来计算不同岩性的速度剖面和预计5000范围内可能岩性界面处的反射系数剖面。 -m中国大陆科学钻探计划(CCSD)地壳部分。计算的原位速度与各自的固有速度的比较表明,浅深度的原位速度由于开放微裂纹的增加而降低。东海钻探区下方的强反射带可以用不同岩性之间的阻抗对比来解释。榴辉岩/橄榄岩和长英质岩石(gt-片麻岩,花岗片麻岩)之间的接触尤其会引起强烈的地震反射。此外,剪切引起的(与晶格优选取向(LPO)相关的)地震各向异性可以提高反射率。为了解释1000 m左右和3200-m以下深度的高速物体(> 6.4 km / s),需要大量的榴辉岩/橄榄岩(分别为40%和30%(体积))。 (C)2002 Elsevier Science B.V.保留所有权利。 [参考:37]

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