Sixteen core samples of siltstone, limestone, metaseds and conglomerate were measured to determine the change of rocky permeability with temperatures.
英
美
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摘要對儲層粉砂巖、灰巖、變質(zhì)巖和礫巖滲透率受熱變化規律進(jìn)行了實(shí)驗研究,并對巖石滲透率在高溫作用下發(fā)生變化的機理進(jìn)行了討論。
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