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钻孔千斤顶压裂测量技术的发展和原地测量 被引量:3
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作者 Yokoyama T Ogawa K +6 位作者 Sano O Hirata A Mizuta Y 徐伟(译) 张雷 姚瑞 沙鹏(校) 《国际地震动态》 2011年第1期67-76,共10页
为了测量距地表1 000m以下位置的地壳应力状态,我们研究并开发了钻孔千斤顶压裂技术。技术的原理是:当钻孔千斤顶对钻孔壁加载时,与钻孔轴向平行的方向将会产生两个相对的新裂隙;卸载之后,如果千斤顶对钻孔壁的同一个地方进行施压,这对... 为了测量距地表1 000m以下位置的地壳应力状态,我们研究并开发了钻孔千斤顶压裂技术。技术的原理是:当钻孔千斤顶对钻孔壁加载时,与钻孔轴向平行的方向将会产生两个相对的新裂隙;卸载之后,如果千斤顶对钻孔壁的同一个地方进行施压,这对裂隙将会再次张开。与钻孔轴向垂直的平面上的两个主应力的大小和方向分别是由重张压力和裂隙的方向决定的。这个技术与水压致裂法相似。因此,测量深度没有理论上的限制。这个技术的特点就是它可以产生一对任意方向的轴向裂隙,可以测量裂隙张开的位移大小,根据测量结果可以精确计算重张压力的大小。在实地测试中,先用水压致裂法形成裂隙,再用钻孔压力千斤顶法加以与水压近似相等的压力值使之重张。本文介绍了我们的数值分析结果、实验室实验和现场测试。 展开更多
关键词 钻孔千斤顶 测量技术 压裂技术 水压致裂法 重张压力 实验室实验 应力状态 测量深度
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In Search of the Cretaceous-Tertiary Boundary in Heilongjiang River Area of China 被引量:15
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作者 Sun G. M.Akhmetiev +18 位作者 Dong Z.M. A.R.Ashraf Sun Y.W. E.Bugdaeva D.L.Dilcher L.Golovneva I.Harding K.Johnson T.Kezina T.Kodrul LU J.S. V.Markevich H.Nishida H.Okada Park S.O. Sun C.L. Xiong X.Z. Xing Y.L. Zhou Z.L. 《Global Geology》 2002年第2期105-113,共9页
A new geological section recognized in Baishantou of Jiayin,Heilongjiang Province,China,was studied preliminarily in searching for the K/T boundary.An early Paleocene florule characrerized by abundant Tiliaephyllum ts... A new geological section recognized in Baishantou of Jiayin,Heilongjiang Province,China,was studied preliminarily in searching for the K/T boundary.An early Paleocene florule characrerized by abundant Tiliaephyllum tsagajanicum leaves and its associated plants,was collected from the Baishantou Member(new member representing the lower part of the Paleocene Wuyun Formation)overlying the possible K/T boundary.A tuff bed was found from the upper part of the Furao Formation(uppermost Cretaceous)in this section.The new findings imply that the K/T boundary is probable lying in the interval between the base of the Baishantou Member and the tuff bed,based on the correlation of the present strata with the stratotype of the Tsagajan Group spanning the K/T boundary in"Belaya Gara"of the Bureya Basin,Russia.The early Paleocene florule from the Baishantou Member and the early-middle Maastrichtian dinosaurs found from the Yuliangzi Formation underlying the Furao Formation suggest that the Baishantou section is more promising for searching for the K/T boundary in this area.Further studies of the section is needed,integrating paleontological,biostratigraphic,geochemical,paleomagnetic,and sedimentary research would benefit our understanding the mass extinction event and biotic recovery in the Heilongjiang River area,China,and even all of northeast Asia during the K/T boundary interval. 展开更多
关键词 K/T BOUNDARY EARLY Paleocene Baishantou MEMBER Jiayin Heilongjiang RIVER
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