Small areas of the waxy crust may dry and flake off, but it is important not to scratch or pick at it, in case infection develops.

小領(lǐng)域的糯 crust 可能缺水和鱗片小康日韩精品91，但它是重要的是不要從頭開始或選擇它，在個案感染的發(fā)展久久久久久久久毛片。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根據(jù)Ar-Ar熱年代學(xué)研究有亚洲一级黄色视频，精確測定了早二疊世伸展變形和晚二疊世擠壓變形的峰期時代分別為290Ma和259Ma.2、提出了關(guān)于哈爾里克山南麓小鋪一帶變質(zhì)帶和變質(zhì)作用的新認識根據(jù)顯微觀察資料和特征變質(zhì)礦物的出現(xiàn)在线观看免费麻豆AV，把小鋪一帶的變質(zhì)巖由SW向NE方向依次劃分為黑云母帶91精彩视频、石榴石帶、十字石帶激情综合婷婷丁香五月、紅柱石帶和矽線石帶等變質(zhì)帶人人干人人射人人；初步確定該區(qū)的變質(zhì)作用屬于中溫-低壓型，變質(zhì)作用發(fā)生的時代為290Ma左右成网站免费在线观看，是該區(qū)早二疊世地殼伸展的產(chǎn)物欧美老妇女操逼视频看看。3、首次提出哈爾里克山南麓在石炭紀可能發(fā)育弧后盆地的新觀點根據(jù)哈爾里克山南麓原"居里得能組"巖屑砂巖的碎屑鋯石SHRIMP U-Pb定年欧美日韩国产风俗，確認這套地層的沉積不早于晚泥盆世国产日B视频网站，很可能是石炭紀，而不是前人所說的前寒武紀国产一区清纯美女在线观看；結(jié)合對其區(qū)域地質(zhì)背景国产h视频网站在线视频、源區(qū)位置和沉積環(huán)境分析，推測該區(qū)石炭紀可能為滯后弧后盆地和弧后隆起區(qū)構(gòu)造背景欧美不卡一区二区三区手机。4最新亚洲日韩中文字幕在线播放一区二区、進一步證明哈爾里克山不發(fā)育與島弧演化相關(guān)的泥盆紀巖漿活動根據(jù)對代表性閃長巖和花崗巖的鋯石SHRIMP年代學(xué)研究獲得的新資料，結(jié)合該區(qū)已有相關(guān)資料的綜合研究全国在线无码精品，確定哈爾里克山巖漿巖分別形成于奧陶紀-志留紀和石炭紀晚期-二疊紀乱子国产刺激，不存在泥盆紀的巖漿巖，進而認為該區(qū)泥盆紀不屬于島弧環(huán)境bbixx.com。5直接在线观看黄色视频主页、重建了哈爾里克山古生代以來的地質(zhì)演化過程根據(jù)區(qū)域資料以及本次研究所獲得的資料，把哈爾里克山古生代以來的構(gòu)造演化劃分中奧陶世-早志留世為島弧国产色视频一区、中志留世-晚泥盆世為弧后區(qū)亚洲热在线视频店、石炭紀弧后伸展、二疊紀為后碰撞伸展與擠壓日韩欧美中文精品第一页、中生代差異隆升和晚新生代陸內(nèi)再造山過程等構(gòu)造階段黄A及黄色视频。6欧美、日韩、亚洲、中文视频、初步估算了哈爾里克山地殼縮短率和縮短量根據(jù)前中生代地層褶皺估算的哈爾里克山南山口-口門子、石城子-白石頭和沁城-小鋪三條剖面的地殼縮短率分別為16.2%国产黄色水国产黄色视频、19.8%和20.1%国产精品一级AAAAAA片在线看，相應(yīng)的地殼縮短量分別為4.3km、9km和11.3km黄色网页视频在线观看。

Evapotranspiration value and transpiration indexes of the three types of soil microbiotic crust under different water content(including Bryum argenteum crust,Didymodon nigrescens crust and algal crust) were measured.

通過對3種土壤生物結(jié)皮在對照和3個不同水分條件下進行蒸散量以及蒸騰指標的觀測国产婷婷网站导航，結(jié)果表明：①3種土壤生物結(jié)皮蒸散量日變化過程呈現(xiàn)單峰型，各個處理間峰值出現(xiàn)時間和蒸散量變化幅度差異較大欧美69av；真蘚對照組峰值為0.473 g/10 cm2国产福利在线99，出現(xiàn)時間為11：00時。

The characteristics of elements shows that magma of fine dioritequartz diorites derived from the enriched mantle or lower crust undergone ocean crust subducting and dehydrating, and was formed and emplaced in the process of crust growth. The magma of dioritic porphyritedacitic porphyries emplaced relatively late, it might derive from upper crust or undergo intensive contamination of crustal materials, and was formed in the proces of crust thining. These characteristics suggest that the geodynamics background of the Jinchanggouliang gold deposit formation is the transition process from compression to extension.

元素地球化學(xué)特征顯示：細晶閃長巖-石英閃長巖的巖漿源于富集地峥梢灾苯用夥压劭吹幕粕罚或洋殼俯沖脫水交代的下地殼一级毛片A片免费播放，地殼增厚過程產(chǎn)生并就位；閃長玢巖-英安斑巖類的巖漿就位相對晚亚洲性h视频在线观看，來源具有上地殼性質(zhì)或被地殼物質(zhì)強烈混染久久久毛片久久久，地殼減薄過程形成；這種特征暗示金廠溝梁金礦形成的地球動力學(xué)背景是在地殼擠壓增厚轉(zhuǎn)化為伸展減薄過程好吊操97在线视频。

From the Late Carboniferous to the Permian, Junggar region into the post-collision tectonic evolution stage, in the stage of the post-collision, the early subduction slab rupture and separate, asthenosphere decompression melting, basalt magma take place underplating, because the underplating of the basalt magma, low crust melt by the high temperature forming the acid crust-magma, the basic magma from mantle and acid one from crust mixing at the vicinity of the crust-mantle boundary, formed the Huangyangshan magma mixing plution, the dioritic microgranular enclaves are the recorder of the crust and mantal magma mixing process.

從晚石炭世到二疊紀黄片拍拍视频免费视频强奸，準噶爾地區(qū)進入后碰撞構(gòu)造演化階段，在后碰撞構(gòu)造階段久久九九手机板看a片免费视频，早期的俯沖板片斷離免费无码不卡a片，軟流圈減壓熔融，玄武質(zhì)巖漿底侵至下地殼底部操人免费网站，底侵基性巖漿帶來的巨大熱量97爱爱，導(dǎo)致地殼物質(zhì)熔融，形成大規(guī)模的花崗質(zhì)巖漿国产原创激情在线观看网站视频下载，兩種巖漿在殼-幔邊界附近發(fā)生不同程度的混合欧美高清不卡A片快爽，其中閃長質(zhì)微細粒包體就是基性的幔源巖漿和酸性的殼源巖漿不同程度的混合的記錄者。

The geological and geophysical data show that in the lower crust of young continental tectonic units may occur pervasive, non-seismic, subhorizontal and ductile flow related to thermal softening. The laminar flow drives fault-block movement of the upper crust, results in the formation of orogenic belts and sedimentary basins, and causes coupling between ductile lower crust and brittle upper crust/mantle.

大量的地質(zhì)和地球物理資料表明国内美女精品人AV在线播放，年輕的大陸構(gòu)造活動區(qū)的下地殼可能因熱軟化而出現(xiàn)透入性非地震式順層韌性流動欧州免费AV午夜福利，這種下地殼層流作用驅(qū)動大陸上地殼發(fā)生地震式脆性斷塊運動日韩揉揉人人澡澡人人，形成盆山格局99精品视频在线看，發(fā)生圈層耦合。

Based on the regional tectonic evolution, combined with the high precision isotopic ages from this paper and other geologists, we have some new acquaintances as follows: 1 There has no Caledonian granite belt distributed in north margin of North China Craton. So, the traditional evolving model of North China Carton, which formed on this idea and the acquaintance about the collision of North China plate and Siberian plate, must be incorrect; 2 The age date show that the earliest magmatic activity began since late-Palaeozoic Permian, which is inconsistent with the previous idea that there were Caledonian and Hercynian active continental margin in the north of North China Craton and in the south Xingkai Massif. 3 the crust and lithosphere were thickened by the subduction and collision of Siberia plate and North China plate during Late Paleozoic. The magma is formed when the crust is heated and melts caused by thickened lithosphere delamination and caused the Asthenosphere upwelling. But only a little basaltic magma erupted, most magma underplate under the bottom of the crust. Thermal energy derived from basaltic magma underplating made the middle and lower crust melt partially and the late Permian-early Triassic granites is formed in large scale.

根據(jù)區(qū)域構(gòu)造演化分析欧美一区二区一页，并結(jié)合本文及他人高精度同位素年齡黑人欧美视频，我們對延邊花崗巖形成的大地構(gòu)造環(huán)境有了新的認識：1在華北地臺北緣并不存在所謂的加里東花崗巖帶，因此欧美色日韩，建立在此之上的傳統(tǒng)的華北地臺北緣演化模式及有關(guān)西伯利亞板塊與華北板塊的碰撞拼合的認識也必然是不正確的韩国Ⅴ欧洲V日本VA片在线观看；2華北地臺北緣和興凱地塊南緣不存在加里東期和海西期花崗巖帶黄色网站国产网址，表明兩地塊邊緣最早的花崗質(zhì)巖漿活動始于晚古生代的二疊紀，即不存在傳統(tǒng)觀點所認為的加里東期或海西期活動陸緣欧美久久精品影院一本到综合；3晚古生代由于西伯利亞板塊與華北板塊的俯沖碰撞亚洲天堂第一av，致使地殼和巖石圈增厚，導(dǎo)致加厚巖石圈發(fā)生拆沉作用欧美老妇人和小伙子性生交，使得軟流圈上涌欧美综合在线精品第二页，加熱地殼使之熔融形成巖漿，但玄武質(zhì)巖漿少量噴出地表毛片精品視频一区二区三区，大部分底侵于地殼底部亚洲欧美h视频在线观看，形成下地殼高密度的玄武質(zhì)底侵層，玄武質(zhì)巖漿底侵的熱能引起中下地殼廣泛部分熔融特黄又爽又大又粗一级A片，形成大面積分布的晚二疊世—早三疊世花崗巖毛毛黄片一下。

04"Smooth as Butter"(mobs are at around 62.66) While doing this quest, make sure you kill Marauding Crust Bursters until they drop an Eroded Leather Case, which starts "Missing Missive"

&象奶油般光滑&（在62，66附近做）（做任務(wù)時多殺Marauding Crust Bursters（怪物名稱毛片在线播，硬殼劫掠爆裂者免黄色网页网站？）以打出一件&被侵蝕的皮外套&可以觸發(fā)&丟失的公文&（這個任務(wù)以后在15，52交還

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根據(jù)Ar-Ar熱年代學(xué)研究成年人在线观看，精確測定了早二疊世伸展變形和晚二疊世擠壓變形的峰期時代分別為290Ma和259Ma.2人人妻人人干、提出了關(guān)于哈爾里克山南麓小鋪一帶變質(zhì)帶和變質(zhì)作用的新認識根據(jù)顯微觀察資料和特征變質(zhì)礦物的出現(xiàn)，把小鋪一帶的變質(zhì)巖由SW向NE方向依次劃分為黑云母帶在线免费免费观观看看的黄色视频、石榴石帶人人插人人透人人射人人色人人干、十字石帶、紅柱石帶和矽線石帶等變質(zhì)帶色黄视频污；初步確定該區(qū)的變質(zhì)作用屬于中溫-低壓型国产一在线精品自产拍，變質(zhì)作用發(fā)生的時代為290Ma左右，是該區(qū)早二疊世地殼伸展的產(chǎn)物91视频日韩。3无码专区无码专区、首次提出哈爾里克山南麓在石炭紀可能發(fā)育弧后盆地的新觀點根據(jù)哈爾里克山南麓原&居里得能組&巖屑砂巖的碎屑鋯石SHRIMP U-Pb定年，確認這套地層的沉積不早于晚泥盆世亚洲久久青草鸭，很可能是石炭紀精品无码三级在线视频网站，而不是前人所說的前寒武紀；結(jié)合對其區(qū)域地質(zhì)背景自拍日韩动漫欧美在线观看视频网站、源區(qū)位置和沉積環(huán)境分析AI中国一级无码黄片，推測該區(qū)石炭紀可能為滯后弧后盆地和弧后隆起區(qū)構(gòu)造背景。499re在线观看视频这里只有精品、進一步證明哈爾里克山不發(fā)育與島弧演化相關(guān)的泥盆紀巖漿活動根據(jù)對代表性閃長巖和花崗巖的鋯石SHRIMP年代學(xué)研究獲得的新資料www.成年人黄色污污网站，結(jié)合該區(qū)已有相關(guān)資料的綜合研究，確定哈爾里克山巖漿巖分別形成于奧陶紀-志留紀和石炭紀晚期-二疊紀，不存在泥盆紀的巖漿巖免费一级A片26分钟，進而認為該區(qū)泥盆紀不屬于島弧環(huán)境久99www。5、重建了哈爾里克山古生代以來的地質(zhì)演化過程根據(jù)區(qū)域資料以及本次研究所獲得的資料日本全黄在线视频，把哈爾里克山古生代以來的構(gòu)造演化劃分中奧陶世-早志留世為島弧好大好硬好爽高潮日韩喷水在线、中志留世-晚泥盆世為弧后區(qū)、石炭紀弧后伸展3p视频免费视频、二疊紀為后碰撞伸展與擠壓国产目拍精品一区二区、中生代差異隆升和晚新生代陸內(nèi)再造山過程等構(gòu)造階段。6日韩精品一区在线播放视频、初步估算了哈爾里克山地殼縮短率和縮短量根據(jù)前中生代地層褶皺估算的哈爾里克山南山口-口門子人人插人人人人操人人爽、石城子-白石頭和沁城-小鋪三條剖面的地殼縮短率分別為16.2%、19.8%和20.1%国产盗摄偷窥在线，相應(yīng)的地殼縮短量分別為4.3km初高中精品视频进入、9km和11.3km。

According to the literatures about the gold contents in crust, rocks and sediments published in recent 15 years and a huge amount of reliable analytical data in the study about crust and rocks accumulated, it is recommended that the gold abundance in the crust and in the exposed crust are 1.0 and 0.8 ng/g, the average contents of gold in rocks, igneous rocks, sedimentary rocks and metamorphic rocks are 0.9, 0.6, 1.0 and 1.0 ng/g, the average contents of gold in stream sediments, flood plain sediments, shallow sea sediments and soils in China are 1.4, 1.6, 1.2 and 2.0 ng/g, respectively.

根據(jù)近15年來發(fā)表的大量有關(guān)金在地殼97人人草,人人干、巖石和沉積物中含量的文獻5566亚洲制服丝袜先锋，結(jié)合作者在地殼與巖石研究中積累的金的大量可靠數(shù)據(jù)，綜合給出金的地殼豐度為1.0ng/g中文字幕在线网，出露地殼豐度為0.8ng/g欧美性爱操妣，金在巖石、火成巖2021天天做夜夜爽网站、沉積巖和變質(zhì)巖中的平均含量分別為0.9中文字幕亚洲欧美专区、0.6、1.0和1.0ng/g国免费自拍视频，金在中國水系沉積物白白色在线免费观看、泛濫平原沉積物、淺海沉積物和土壤中的平均含量分別為1.410pao永久免费视频、1.6国产免费看色操日人、1.2和2.0ng/g。