Major conclutions from this study can be summarized as following:1. On mineralogy, rutiles, apatites, epidotes and vein minerals from UHPM rocks were firstly and systematically studied, by detailed petrography and mineral-chemistry investigation, some mineral or mineral assemblage with special composions or texture were firstly found in UHPM rocks from Sulu-Dabie, for example, corrudum, magnesite, high-Ti biotite and garnet were found as inclusions in rutiles from eclogites, Nb-Fe rutile and zoned Si-Y apatite were found in gneiss, epidote / allanite with euhedral zones like magmatic genesis were found in elogites and gneiss, a lot of minerals with high REE, HFSE, LILE and volatiles were found in veins of gneiss.

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Two genetic types of dawsonite, namely inorganic and organic are divided in response to origin of carbon dioxide. Inorganic genesis includes magmatic origin and carbonate decomposition origin.

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A complex suite of intermediate-basic to intermediate-acid and relatively alkaline volcano-intrusive rocks of dominant andesitic composition and a group of iron ore deposits of somewhat different genetic types associated with them, including late magmatic, pegmatitic, pneumato-hypothermal, pyrometasomatic, meso- to epithermal deposit and the possible ore-magmatic and volcanic-sedimentary deposits, which are the successive products of the magmatic evolution, widely distributed in the faulted basins in the mi...

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The activities in different sections of the Gaoqing fault in the Huagou gas field were analyzed using 3D seismic data. The activities of the fault segment associated with the Huagou gas field were strong during the Guantao\|Minghuazhen period, while the activities on east and west sides of the gas field were weak at that time. The Huagou gas field is well corresponding to the strong activity segment of the Gaoqing fault on the plane. The process of gas migration in the Huagou reservoir is divided into two phases:(1)After mantle\|derived magmatogenetic gas including CO2, N2, and He entered the Gaoqing fault, the gas migrated to the top of the fault by the action of buoyancy or pressure, then the gravitative differentiation occurred. For the top of the fault is closed and both sides of fault is sealed, the gas assembled to some degree in the Gaoqing fault;(2)When gas was accumulated at a large scale in the Gaoqing fault, the gas migrated towards the reservoirs along the two sides of the fault and was accumulated in sandstone.

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This article is on the basis of the predecessors working results. After a thorough and meticulous field geological survey ,it collects a large number of geology information and researches from the regional metallogenic geological background, and focuses on the formation, structure, palaeogeographic environment and mineralization. It describes the nature of the deposit, evolution and the formation of the ancient environment,analysis of the source material,sedimentary environment, advises the genesis point of view and establishes the deposit model,studies the control factors and bauxite ore mineralization, sums up the mineralization law and suggests the favorable prospect of this area.

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ACCD has induced five characteristics in sports training, which are the pluralism and changeable origin cause, guiding physique, controllability and uncontrollability of variation course ,the two polarities and level of the result and the mutability of the perform behavior.

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Skill-mental dominated event-group has characteristics what are polarizing frighten goal and fluctuating variation course. 6 Coaches and athletes must insist on the principles that is comminuting of judging accurately and intervening in good time, perspective with getting practical to combine together, timeliness and synchronous combine together, controllability and principle that substantial results combine together.

影響競賽過程中運動員競技能力變異的眾多因素可聚合為以下四個相對獨立又相互聯(lián)系的子系統(tǒng)，即：運動員的競技狀態(tài)與相對競技實力95香蕉视频、參賽認知水平與比賽經(jīng)驗日本乱人伦A片免费高清、可逆轉(zhuǎn)環(huán)境和中立環(huán)境。4運動員競技能力的參賽變異具有變異成因的多元性和多變性国产美女在线精品免费观看网站污、變異內(nèi)容體能的先導(dǎo)性思思99精品视频、變異過程的可控性與非可控性、變異結(jié)果的兩極性和層次性和參賽行為的心態(tài)易變性等五個方面的一般訓(xùn)練學(xué)特征日韩一级啪啪啪啪啪啪。5體能主導(dǎo)類項群具有變異結(jié)果直觀性国产无码乱伦午夜、變異過程連續(xù)性和對手制約兩重性等特征；技能主導(dǎo)類項群具有單項貢獻制約性久久免费看黄视频、個體變異傳遞性和裁判評定誘導(dǎo)性等特征88色哟哟；技戰(zhàn)能主導(dǎo)類項群具有群體整合共生性、核心技戰(zhàn)術(shù)制導(dǎo)性亚汌人成伊人成综合网222、攻防轉(zhuǎn)換制約性和局盤賽點突增性等特征人人爱人人操人人搞；技心能主導(dǎo)類項群具有目標(biāo)恐懼極化性和變異過程波動性等特征。6教練員日本特级特黄aaaa大片、運動員必須堅持準(zhǔn)確判斷和適時干預(yù)相結(jié)合蝌蚪网在线视频、前瞻性與務(wù)實性相結(jié)合、適時性與同步性相結(jié)合aaaa片、可控性與實效性相結(jié)合的原則A片无卡不码国产在线。

Ana lyses of the main shale gas basins in America show that gas shale reservoirs can be classified into thermal genetic type.

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Huangqiao carbon dioxide gas field in North Jiangsu Basin have the following characteristics: deep gas fields are associated with shallow ones, marine gas fields are coupled with continental ones, and several gas reservoirs are combined. Carbon dioxide in Huangqiao area mainly comes from deep mantle, mixed with a little thermal metamorphism and a little organic carbon dioxide in shallow formation, and helium and nitrogen gas mainly come from mantle. There is a good time\|space matching relationship between carbon dioxide gas reservoirs and great rifts, magma and volcano activity, which forms the special carbon dioxide gas reservoir mode for Huangqiao. This mode has good sealing, trapping and preserving conditions, but its gas source differs from traditional hydrocarbon gas reservoirs.

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On the basis of summarizing the status quotation of related researches at home and abroad, problems in related researches and studies are analyzed and the important research fields and contents in marsh sedimentology are chosen:Establishing different model of marsh sedimentation, to support marsh definition and classification from sedimentology; Advancing theory and quantification, to analyze formation process of marsh from quality to quantity methods; Applying modern sampling system and setting up standard sedimentation profiles; Strengthening the research of gleying marsh inland and its recent process and evidence derived from sedimentation profile; Enlarging geography fields and comparing between spatial and temporal research, and enforcing regional short timescale and highresolution environmental change; Paying much more attention on correlations between watershed environment and information derived from marsh sedimentary records and especially on their controlling mechanism.

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