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Density of UHP Metamorphic Rocks from CCSD Main Hole

机译:CCSD主孔超高压变质岩的密度

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摘要

For learning the densities of UHP metamorphic rocks and the differences between logging and core test density, this study displayed the density profiles obtained by well logging and core test at the 5 000 m deep CCSD-MH (Chinese Continental Scientific Drilling Main Hole), compared log density with core's. The upper section (100-700 and 1 600-2 000 m) of CCSD-MH, which consists of mainly eclogite and amphibolite, displays high densities (2.8-3.6 g/cm3). The lower section (2 000-5 000 m), which consists of mainly orthogneiss and paragneiss, displays low densities (2.6-2.7 g/cm3). The retrogression lowered the density of eclogite. Thus the density profile of CCSD-MH was mainly governed by lithologies. The variation of log density was coherent with that of core test on the whole, and the log density was a little lower than core's. The density log is severely affected by the cavings and breakouts of borehole, so it is necessary to correct the density log properly.
机译:为了了解UHP变质岩的密度以及测井和岩心测试密度之间的差异,本研究显示了在5000 m深CCSD-MH(中国大陆科学钻探主孔)处通过测井和岩心测试获得的密度剖面,对数密度与核芯。 CCSD-MH的上部(100-700和1600-2 000 m)主要由榴辉岩和角闪石组成,密度高(2.8-3.6 g / cm3)。下部(2 000至5 000 m)主要由生正片麻状岩和扇形岩构成,密度较低(2.6-2.7 g / cm3)。倒退降低了榴辉岩的密度。因此,CCSD-MH的密度分布主要受岩性控制。总体上,对数密度的变化与岩心试验的变化一致,对数密度略低于岩心的密度。井眼的崩落和破裂会严重影响密度测井,因此有必要正确校正密度测井。

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