For the status of the fishing technology of deep and ultra-deep slim hole was started later, the lack means of dealing with accidents and little fishing experience on the oil field, from the actual conditions of the Tarim oil field and in research on the basis of information at home and abroad, this article analyzed the technical difficulties of fishing in the deep and ultra-deep Slim hole and the importance of preparations before fishing, and then summarized the powdered magnesium technology, sets milling fish-neck technology , Venturi joints with milling technology and fishing rope-type fish with spiral bailer grab technology.

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The eight major research topics are :①understanding coremantle processes, by deep drilling into a large oceanic plateau in the Western Pacific;②detailed investigation of material circulation during greenhouse Earth, and the transition process from greenhouse to icehouse environments, by drilling Cretaceous to Cenozoic sediments in the Pacific,③understanding the process of continental crust formation by deep drilling into oceanic arc,④Understanding the process of oceanic lithosphere formation by deep drilling of the back arc spreading system,⑤understanding of continentoceanatmosphere linkage, by drilling in the marginal seas and continental slopes of Asia,⑥investigation of the carbon cycle and the deep biosphere in accretionary prisms,⑦investigation of the mechanism and cycles of great earthquakes, tectonics, and mass circulation in convergent plate margins,and ⑧biology of extreme microorganisms living in deep accretionary prism environment.Keywords : Japan IODP Drilling Scientific goals.

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The deep water deposition means the deposition in the area where the water depth is larger than 30 meters, in which the major sediments are coarse sand and gravel. This kind of deposition is the relic deposition formed by the Pleistocene alluvial-lacustine deposition reworked under modern channel currents actions, and ususally the Holocene acummulation lack in the deep waters. The transitional zone deposition is the deposition between the low tidal level line and the 30 meters isobath, where the sediment types is changeable and the grain sizes are gradually coarsening from the low tidal line to the deep water area. This kind of deposition is developed by the deep water eroded sediments sorting under the transitional zone current action. The different types distributed along the isobath. The tidal flat deposition is the fine sediment deposition on the tidal flat which is flo sedimentation of the silty clay under the tidal flat dynamic action and ususally developed fluid mud on the lower tidal flat. The channel mouth deposition is the deposition in the channel mouth area. According to the sediment types, it includes sand deposition where there are coarse sediments supply and silt deposition where there are only fine sediments surpport.

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The constant nutritional arteries of the great saphenous vein-saphenous nerve on the medial foot: Perforator at medial side of the tendon of the tibialis anterior ,it is （2.27±0.43）cm distal to the intermalleolar line .it passes across the medial side of the tendon of the tibialis anterior and pierces the deep fascia between the upper and lower bundle of the inferior extensor retinaculum with a diameter of （0.72±0.04）mm;The length of it after piercing the deep fascia is （7.3±0.6）mm,It has an emerging rate of 95%; Perforator between tendons ,it is （3.02±0.39）cm distal to the intermalleolar line;it pierces the deep fascia between the tendons of tibialis anterior and extensor digitorum longus with a diameter of (0.57±0.06)mm ;The length of it after piercing the deep fascia is （7.4±0.6）mm .It has an emerging rate of 94%; A constant distal fascial perforator pierces the deep fascia between abductor hallucis muscle and medial side of first metatarsal bone （1.97±0.23）mm distal to the first metatarsophalangeal joint with a diameter of (0.50±0.03)mm.

足內(nèi)側(cè)大隱靜脈-隱神經(jīng)營養(yǎng)血管近端來自內(nèi)踝前動(dòng)脈較為恒定，外徑較大的穿支有：踝間線遠(yuǎn)端（2.27±0.43）cm日韩天堂免费视频在线，經(jīng)脛骨前肌腱內(nèi)側(cè)人人摸'人人操人人、伸肌下支持帶上、下束間穿出中国区第一黄色网，外徑(0.72±0.04)mm 久久精品国产字幕AV，穿出深筋膜的長度為（7.3±0.6）mm，出現(xiàn)率為95%美国黄色视频黄色视频聊天；踝間線遠(yuǎn)端（3.02±0.39）cm6080新觉伦午夜理论无码，經(jīng)脛骨前肌腱與趾伸肌腱穿出，外徑(0.57±0.06)mm超碰91成人人做人人爱，穿出深筋膜的長度為（7.4±1.2）mm 最新国产三級片，出現(xiàn)率為94%；3遠(yuǎn)端來自交通支最為恒定，外徑較大的穿支于踇展肌與第一跖骨內(nèi)側(cè)緣之間穿出深筋膜无遮无挡爽爽免费视频毛片，距第一跖趾并節(jié)近端（1.97±0.23）cm91cao，直徑（0.50±0.03）mm，穿出深筋膜的長度為（6.5±0.5）mm午夜视频www，出現(xiàn)率為100%欧美性爱视频一日本高清视频。

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Thus, based on analysis and situ-survey in Zhoushan area, some proposals are put forward on utilization of marine resources in Zhoushan Archipelago:(1) The deep shoreline resources can be used to build international deep-water port for transferring raw materials such as metal ore, coal, and crude oil. Furthermore, they can be also built up as a process industry base relying on harbor for staple goods and a standby deep-water port for transporting goods of the Yangtze River Delta outward.(2) There is a great potential on the development of deep water aquaculture and offshore fishing.(3) It is an appealing resort for marine tourism especially in holiday relaxation which supplies the gap of tourism in the Yangtze River Delta.

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This article analyses the application conditions of freezing method, current research status and the problems in this field. It points that it's necessary to study deep freezing temperature field deeply and discusses the factors which influence the freezing wall such as soil's nature, moisture content, geological conditions, etc. It introduces the theory, process of freezing method, the distribution of temperature field of freezing method and key thermotics parameters influencing freezing temperature field. It simplifies the deep freezing temperature field model. Through ANSYS, this article founds the deep freezing temperature field model, and simulates the field on vary heat conductivities. It analyzes the results of ANSYS simulation, gains the theoretical value of thermometric holes which is needed by back-analysis. Using the simulation temperature and actual value, it gets the equivalent heat conductivity. Then it solves the deep freezing temperature field by the equivalent value, simulates the freezing wall development process and temperature change curve. Against the actual project, the results are favorable.

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