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1.2. In flat dip layer, the seam thickness control the stability of the wall rock, the thick-bedded hard rock is stable than the thin-bedded hard rock.
② 岩层度在缓倾斜时对围岩稳定起控制作用,层硬岩整体稳定性好于薄层状硬岩。收藏指正
2.Some syndepositional soil-layers disturbed by earthquakes were discovered in thick-bedded alluviums of Eocene Zhubidian formation in Anqiu area of Tancheng-Lujiang seismic zone.
摘要在郯庐地震带的安丘地区,发现始新世朱壁店组层冲积层中发育一些同沉积的地震扰动岩土层。收藏指正
3.There exists a succession of shallow-water,thick-bedded carbonate sediments a few hundred meters thickabove the Middle Triassic Sanbao’ao Formation in southeastern Hunan.
湘东南区的中三叠统三宝坳组之上,存在一套数百米的浅水层碳酸盐岩沉积。收藏指正
4.Orobodies strike SE, dip NE and have dip angles 70°-80°. Host rocks are yellowish green and black serpentinites and serpentinized marble, with thick bedded hydrothermally deposited laminar tourmalite also seen in the hanging wall of the orebodies.
矿体走向SE,倾向NE,倾角70°~80°,直接赋矿岩石为蛇纹岩、蛇纹石化大理岩,矿体顶板出现有热水沉积的电英岩。收藏指正
5.The strata of this area are divided in ascending order as fllows: 1.Shiqianfeng Group:It is subdivided in three formation(ascending order as follows). (1)Sunjiagou Formation(p_2s):The basal part is dominated by thick-bedded greyish white,yellowish white coarse sandstone.
该区的地层自上而下划分如下:1.石千峰群:可进一步分为三个组(自下而上):(1)孙家沟组(P_(2s)):底部为灰白、黄白色粒砂岩;收藏指正
6.Analysis of the sporopollen record and regional geological data indicates that the thick-bedded conglomerate in the upper part of the Kokyar section should be early-middle Pliocene in age,while the deposition of the entire molasse should begin still earlier,i. e.
孢粉记录结合区域地质资料分析表明,柯克亚剖面上部层砾岩的形成时代应为上新世早中期,而整个磨拉石开始沉积的时代应更早,为中新世晚期。收藏指正
7.The Yankou Formation in the Upper Ordovician of Tonglu County in Zhejiang Province consists mainly of rhythmically thin alternating layers of gray fine-grained sandstones, siltstones and dark-gray mudstones, silty mudstones, in which the typical flaser, wavy, lenticular bedding and rhythmic stratification are well developed, with 2-3 intercalated beds of gray medium- to thick-bedded conglomerates in the base of the formation.
浙江桐庐地区上奥陶统堰口组主要为一套灰色细砂岩、粉砂岩与深灰色—灰黑色泥岩、粉砂质泥岩的韵律性薄互层,底部发育2~3层灰色中—层的砾岩,其砂泥岩薄互层中发育有典型的脉状、波状和透镜状层理及韵律层理。收藏指正
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