The outgas types and amount of different gas resource varied with the different geological conditions and evolution processes. There are four outgas models including the model in which inorganic gas directly overflows from mantle matter through lithospheric fracture,the model of heat flow piercement outgas,the model of volcano-magma outgas,and the model of carbonate rock outgas due to heat metamorphism.

對(duì)氣藏成藏條件和深部殼幔結(jié)構(gòu)的研究表明国产肏屄自拍，松遼盆地存在多種類型無機(jī)"氣源"国产古装一级牲交高潮片，由于賦存的地質(zhì)條件和演化過程不同，不同氣源脫氣的方式日韩制服卡通自拍图、脫出氣體的類型一级A片自慰超刺激无码、脫氣量也大不相同，共有4種主要的模式：地幔物質(zhì)沿超巖石圈斷裂直接脫氣模式JIZZ精品国产；熱流底辟體脫氣模式91精品www；火山—巖漿成因模式；碳酸鹽巖熱變質(zhì)成因模式日韩AV无码超碰一区二区三区。

In petrology, fenite and fenitization have been identified,and the existence of igneous carbonatite has been confirmed.

在地球化學(xué)和礦床成因方面一级一级毛片在线看，提出了稀土稀有金屬礦化與火成碳酸巖巖漿活動(dòng)有成因聯(lián)系的見解。

And the late Triassic bimodal association reflects the characteristics of intracontinental rift setting, the early Jurassic Raohe ultramafic - mafic rock - pillow lava association represent the environmental characteristics of oceanic island, magmatic arc association represent the characteristics of island arc and active continental margin with the background of the plate subduction, middle Jurassic syn-orogenic granodiorite-granite association reflects characteristics of matching and orogensis after continental accretion.

其中晚三疊世雙峰式組合反映了板內(nèi)裂谷成因特征6080免费三级片，早侏羅世饒河超鎂鐵質(zhì)-鎂鐵質(zhì)巖-枕狀熔巖組合代表了洋島環(huán)境特征大香蕉日韩亚洲网在线播放，巖漿弧火成巖組合代表了板塊俯沖背景下島弧和活動(dòng)大陸邊緣特征，中侏羅世同造山花崗閃長巖-二長花崗巖組合反映了陸緣增生后拼貼造山的成因特點(diǎn)久久伊人中文字幕色综合，它們總體上代表了由被動(dòng)陸緣裂向活動(dòng)陸緣轉(zhuǎn)化并最終發(fā)生陸緣增生帶拼貼造山的一個(gè)演化過程国产高清在线a视频大全在线，其間伴隨有被動(dòng)陸緣深海盆地沉積、活動(dòng)陸緣弧后前陸盆地沉積和陸相類磨拉石建造

The study on formation cause of plagioclase is closely related to formation cause of geological structure.

對(duì)斜巖成因的研究與人們對(duì)大地構(gòu)造成因的認(rèn)識(shí)密切相關(guān)www.saomz02.com。

The study on formation cause of plagioclase is closely related to people's knowledge on the formation cause of structure of the earth.

對(duì)斜巖成因的研究與人們對(duì)大地構(gòu)造成因密切相關(guān)欧美阿视频99在。

On the basis of a study and elaboration of data, some important conclusions are presented:(1) ruby deposits in marbles occur in the plutonic metamorphic zones of orogens where deep fault structure is developed;(2) ruby-bearing rocks are calcic crystalline marbles, rather than magnesian marbles;(3) amphiboles in ruby-bearing rocks are not tremolites, but silica-poor, alumina-rich and chrome-bearing calcic amphiboles, such as chrome-bearing magnesio-sadanagaites; and (4) the deposits are genetically of thermodynamical metamorphism type, rather than of pneumatolito-hydrothermal type or skarn type.

目前，對(duì)于與此類型礦床找礦相關(guān)的若干成因問題的認(rèn)識(shí)www日本com黄色，還相當(dāng)模糊国产自啪女女，主要表現(xiàn)在以下幾方面：①對(duì)此類型礦床的產(chǎn)出構(gòu)造背景認(rèn)識(shí)不清；②認(rèn)為含礦巖石為鎂質(zhì)大理巖或鎂質(zhì)夕卡巖国产乱伦窝边操；③認(rèn)為含礦巖石中與紅寶石共生的角閃石為透閃石久久99久久99精品欧美男男；④認(rèn)為此類礦床的成因類型為"氣成一熱液型"或"夕卡巖型"。本文在實(shí)際研究(王禮勝美国潢色片AAAwWwA，1996)和文獻(xiàn)資料整理的基礎(chǔ)上性爽交免费视频，分別對(duì)這些問題給予了澄

TOF-SIMS images show bacteriogenic pyrites are relatively rich in Cu, Zn, and Ni, suggesting that bacteria probably play an important role in the enrichment of Cu, Zn, and Ni during their formation.

TOF-SIMS 的離子像亦表明菌落成因的黃鐵礦富集 Cu 、 Zn 和 Ni 一级国产精品毛片视频，表明菌落在生物成因黃鐵礦的形成過程中亚洲色了，在改變介質(zhì)條件99久久国产综合精品婷婷、在遷移、活化和富集 Cu 午夜影院三级、 Zn 等金屬元素方面做出了貢獻(xiàn)91精品视频网。

A The chief "commentaries" on the Old Testament are the sixty-seven homilies "On Genesis"(with eight sermons on Genesis, which are probably a first recension) IV, 21 sqq., and ibid., 607 sqq.

行政"的評(píng)論文章"論舊約是67頌歌"成因"（即八布道成因，這可能是第一次recension ）（四黄片免费看的AAA， 21 sqq 视频一区二区在线观看，并同上， 607 sqq 九九一级黄色视频。

At last,we find the cause of formation of red mud-intercalated by analyzing 4 possible cause of formation : tectogenesis form; natural weathering and relaxtion form; drtion and destroy of slope form; collapse of cavity because of karst affect in the base of investigating istogeological condition of circumscription and dam zone and physiognomy of dam zone.

在調(diào)查掌握區(qū)域和壩址區(qū)地質(zhì)條件以及壩址區(qū)地形地貌的基礎(chǔ)上国产丝袜在线观看视频黄，從四個(gè)方面分析了紅色夾泥的可能成因：構(gòu)造形成、正常風(fēng)化卸荷形成久久久久久久精品电影网、斜坡變形破壞形成以及巖溶溶洞垮塌形成伊人草在线视频，最后得出紅色夾泥的成因。

According to geological characteristics of mineral area,geological conditions of mineralization,geochemical characteristics,material sources of mineralization,mineralization patterns,as well as physical and chemical conditions of mineralization,it summarize the mineralization pattern and genesis of ore deposit of Xianghualing mining areas,considering that mineralization materials in this deposit mainly come from magma,genesis patterns of deposit include high-temperature gas-liquid Nb亚洲无视频区、Ta deposit related to albitization laying in or on the edge of granite rock bodies,median-high temperature Skarn Sn,Be deposit related to skarnized laying at the inner contact-belt of granite and carbonate rock bodies;median-high temperature cassiterite -sulphide mineral deposit related to skamized laying at outer contact-belt of granite and carbonate rock bodies and median-low temperature hydrothermal liquid Pb-Zn-Ag deposit related to silicification,fluorite, propylitization laying in wall rocks;Series of generalized magma- hydrothermal liquid type Sn-polymatellitic related to magmatic activity in Yanshan period as a whole.

通過對(duì)礦區(qū)地質(zhì)特征好爽好大好紧别拔出来视频、成礦地質(zhì)條件、地球化學(xué)特征超碰欧美图片zxxxx、成礦物質(zhì)來源在线高清免费不卡无码黄片、成礦作用、礦化型式以及成礦物理化學(xué)條件的分析天天日天天干天天天添，總結(jié)了香花嶺礦區(qū)的礦床成因以及成礦模式欧美黄片天天在线观看，認(rèn)為香花嶺錫多金屬礦成礦物質(zhì)主要來源于巖漿，礦床成因類型包括花崗巖體內(nèi)及其邊部產(chǎn)出的與鈉長巖化有關(guān)的高溫氣液型Nb五月丁香花婷婷综合、Ta礦床男女人精品视频站在线观看、花崗巖體與碳酸鹽巖內(nèi)接觸帶產(chǎn)出的與矽卡巖化有關(guān)的中高溫矽卡巖型Sn、Be礦床亚洲精品一、花崗巖體與碳酸鹽巖外接觸帶產(chǎn)出的與矽卡巖化有關(guān)的中高溫錫石硫化物礦床以及圍巖中產(chǎn)出的與硅化亚洲色图五月天综合、螢石化、青磐巖化有關(guān)的中低溫?zé)嵋盒豌U鋅銀礦床网页升级自拍偷拍，整體構(gòu)成與燕山期巖漿活動(dòng)有關(guān)的廣義巖漿熱液型錫多金屬成礦系列