• 基本释义

1.Geological Review of CBM Exploitation in Panguan Syncline,Lupanshui Coalfield,Guizhou
贵州省六盘水煤田盘关向斜煤层气开发地质评价收藏指正
2.The first stage was from Late Caledonides to Early Hercynian Period, and two exposed palaeo-karst types of erosion depression discharge in syncline wings and intermountain depression discharge in syncline axle developed.
第一阶段为加里东晚期—海西早期,发育向斜翼部侵蚀洼地排泄型和向斜轴部山间洼地排泄型古岩溶;收藏指正
3.After later Palaeozoic, this area was transformed into a paraplatform from" southeast Caledonian miogeo- syncline" by later Caledonian movement.
晚古生代始,转化为后加里东准地台。收藏指正
4.SED IMENTARY FACIES OF DEVONIAN PERIOD OF THE WESTERN FLANK OF SIMAQIAO SYNCLINE IN DAO COUNTY,HUNAN PROVINCE
道县四马桥向斜西翼泥盆纪沉积相收藏指正
5.The 3~(rd) depression of Ordos basin came about under the Yanshan movement after the Trias Jura & Jurassic and the center gradually move to the west, which lead to a huge anisomerous syncline of widely slow eastern side and precipitously narrow west.
鄂尔多斯盆地在燕山运动作用下使区内发生了自三叠系和侏罗系后的第三次拗陷,沉降中心不断西移,形成一个东翼宽缓、西翼陡窄的不对称巨型台向斜收藏指正
6.The mineral water occurs in sandshale of Triassic system,structurally near the east-limb of the north part Qinshui syncline,In 1987 and 1993,respectively,the water qualityhad been identified by Shanxi Bureau of Geology & Mineral Resources and Ministry of Geolo-gy & Mineral Resources,It is accordant with national standard of《Potable Natural Mineralwater》(GB 8537-87), and belongs to strontium bearing-metasilicate,bicarbonate-sodiumcalcium type mineral water.
矿泉水赋存于沁水向斜北部东翼三叠系砂页岩地层中,1987年和1993年经山西地矿局和地矿部组织鉴定,水质符合《饮用天然矿泉水》国家标准(GB8537-87),属含锶-偏硅酸重碳酸-钠钙型矿泉水。收藏指正
7.Gouxi structure is a stratigraphic-faulted nose, combination trap, which is bounded by reverse fault at the east side and by the wide Shenjiachang syncline at the west side, covers a large area and lately outcropped, indicating there existed good preservation conditions and a large gas source area, which made the trap becoming a favourable one for gas exploration.
荷西构造为地层一断界复合圈闭,东侧由道断层遮挡,西侧与沈家场宽向斜相接,圈闭面积较大,出露地层新表明保存条件好,气源供给范围大,是有希望获气的有利圈闭。收藏指正
8.The two wings tectonics and metamorphism in Tai Ping-shan syncline were studied by the method of comparison, and it has been proved that the intrusion of Fang Shan magmatic rock was the sources of various geological effects, all different typical geological phenomena are the results of magmatic rock intrusion, and the nearer distance the area to the Fang Shan magmatic rock, the stronger effect it has.
本文通过比较分析的方法,对太平山向斜南北两翼构造变形和变质进行了研究,提出了“房山岩体”的侵入作用是本区各种地质作用的主要动力来源,区内各种典型的地质及构造地质现象是岩体侵入作用的结果,离岩体越近影响程度越大,远离岩体逐渐减弱。收藏指正
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