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岩石

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Study on the petrochmical,trace element chemical,REE geochemical and Pb isotopic geochemical characteristics of the Tongshan intrusive indicates that the quartz diorite,granodiorite and adamellite are products of three stages of the same periodfrom only one magmatic source.

通过岩石化学、微量元素地球化学、稀土元素地球化学、铅同位素地球化学特征研究表明,铜山石英闪长岩、花岗闪长岩、二长花岗岩是同一岩浆源同一时期三个侵入阶段的产物,铜山岩体幔壳同熔型的复式岩体,属太平洋钙碱性岩石系列。

According to comprehensive research of lithogengesis and lithogeochemisty, all these volcanic rocks have higher alkalinity, alkalis with sub-alkalis series, normal type with akali type have coexisted, and SiO2 have oversaturated rock with under saturate.

通过岩石学,岩石地球化学分析,该火山岩整体碱度较高,碱性和亚碱性系列共存,正常类型和钾质类型共存,SiO2过饱和或低度不饱和。K2O平均含量3.4%,K2O/Na2O值多大于0.6,中基性岩Al2O3含量多大于16%。

It is composed of Himalaya period potassic alkalic magmatic rock. The zone is 3700 kilometres.

碱性岩是除幔源岩石包体外另一类可提供地幔信息的岩石,是窥探地幔的窗口。

Being rich in potassium, alkali and calcium, this belt is a series of potassic and alkalic granitoids and belongs to A-type granites. However, this kind of A-type granitoids was not formed at the end of orogeny.

岩石地球化学研究显示,该岩带的各种岩石类型都具有富钾、富碱和富钙的特点,属于钾质碱性花岗岩类,可归属为A型花岗岩类。

It shows that the sedimentary facies are submarine fans deposited by gravity flow at the bathyal depth.

综合应用沉积岩石学、地质学等多学科理论,全面分析了F4层的岩石学性质、沉积构造特征、测井曲线特征、古生物特征等,认为F4层的沉积相为陆隆-半深海环境下重力流沉积的海底扇。

Party ah'ou'' yo wow wrong wanna a chair super negro wanna said hanging out man negro show will love some of a faggot you are murd when i dread to make a connect to yo babies dont try helicopter pipe-check we'll be smoking a cigar so as bad as sharper rocking down somebody everywhere of a party over there man sweetie homie sot all the danstroll mad all train the city cause we the best droll size the rockies to flat by a squash like a super star try to right up at the top whoever say no way, check it out the quality's down whoever like it or moaning out turning our stuff around last night a jewel saved my life, now that all you want last night a jewel saved my life, there's a party going on last night a jewel saved my life, now is bergy time last night a jewel saved my life, there's a party going on now should get down jungle fibre getting tie boogy night we'll be the one and the male smoothy is looking for kill we'll be the top place wrong place raping the world cause we would have top place now start the pub we'll be the hard too, shaking everybody what a tough shit bar man rocks for its tale beating me in the dance and never tell mine too, my thingy got to swing it with me my moving making everybody dance i'll be the dance keep surprising everybody with a jet you taking over your mind cause where the jackets were the baseline checking it hard cause we'll be the place sudden start bald day last night a jewel saved my life, now that all you want last night a jewel saved my life, there's a party going on last night a jewel saved my life, now is bergy time last night a jewel saved my life, there's a party going on now bergy time,bergy time bergy time,bergy time damn number rare yo, yeah, come on ,come on ,come on, come on damn number rare yo moving w yo yo 怎么 boorgy

落某人 为情人 homie 醉鬼配备人手所有的 danstroll 疯狂的所有的训练城市引起我们最好人好笑的对褶皱不堪的公寓按规定尺寸制作岩石者喜欢一个超级星尝试到正确地增加在顶端任何人没有说方法,检查出它质量的下来任何人喜欢它或呻吟出将我们的东西转回头昨晚,一些珠宝节省了我的生活,现在全部你想要昨晚,一些珠宝节省了我的生活,有一个宴会继续昨晚,一些珠宝节省了我的生活,现在是 bergy 时间昨晚,一些珠宝节省了我的生活,有一个宴会现在继续应该拿下来丛林纤维得到领带 boogy 夜晚 smoothy 正在找寻杀我们将会是那一和男性我们将会是最上面的地方错误的地方轻敲世界引起我们会有最高的地方现在开始酒馆我们将会是那努力地也,摇动每个人什么强硬的粪除为它的故事的男人岩石打我在跳舞方面我的感人的使每个人都跳舞我将是跳舞用喷气式飞机保存令人惊讶每个人而且也不再告诉我的,被开始的我的 thingy 和我摇摆它你接管你的思想引起夹克是基线的地方努力地检查它引起我们将会是地方突然开始秃头日子昨晚,一些珠宝节省了我的生活,现在全部你想要昨晚,一些珠宝节省了我的生活,有一个宴会继续昨晚,一些珠宝节省了我的生活,现在是 bergy 时间昨晚,一些珠宝节省了我的生活,有一个宴会现在继续非常的数字稀有的 yo,是的,发生,发生,发生,发生诅咒数字稀有的 yo 迁出 yo 摇摆二十折层取出 yo 飞行 yo 昨晚,一些珠宝节省了我的生活,现在全部你想要

This dissertation was focused on the research about the formation and evolution of NQB from the Late Triassic to the early middle Epoch of Jurassic Period, including integrated analyzing the characteristic of the key stratigraphic surfaces, the time of the key stratigraphy, regional rock straigraphy, biostratigraphy and chronostratigraphy, sedimentary system and depositional facies. On basis of these analysis, a tectonic evolution model have been established for NQB during from the Late Triassic to the early middle Epoch of Jurassic Period.1. After the systematic surface analysis about main stratigraphy units, we found that:(1) the bottom of Xiaochaka formation was comformity with the middle Triassic in the basin, and in the north margin it was deposited and overlapped on the different period stratigraphy before Triassic.(2) The top surface of Xiaochaka formation developed regionally karst and paleo-karst breccia, and was uncomformity with Nadigangri Formation, these things suggest that NQB in Xiaochaka depositing stage was developed from middle Triassic basin, and then an extensive regression occurred, the deposition was over and erosion come into being.(3) The lithologic assemblage, geochemistry, mixed fossils, and stratigraphy overlapping characteristic of Quemocuo Formation in early middle Jurassic indicted that the uncomformity surface was an extension-unconformity.2. Integrated analysis about stratigraphy division and correlation indicted that:(1) the paleontologic assemblage of Xiaochaka formation show its time was Carian -Norian stage of late Triassic. According to it was overlapped by late Triassic Nadigangri Formation, so Xiaochaka formation should be Carian - early Norian stage.(2) the SHRIMP Zircon U-Pb age of Nadigangri formation volcanic rocks wear vary form 216 to 205 Ma, so its time should be Norian, but maybe extended into Rhaetian Stage.(3) The age of its bottom volcanic rocks, the fossil assemblages of its middle and upper members and overlapped by lower Jurassic, indicted the age of Riganpeicuo Formation was Norian - Rhaetian stage. And the same time, the volcanic rocks geochemistry of Nadigangri and Riganpeicuo formation both reflected that they wear formed in rift tectonic settings. The lower lithologic and surface characteristic, fossil assemblages and its upper maybe was conformity with lower Jurassic, all reflected that the age of Tumengela Formation in Tumen area should be Norian - Rhaetian stage.

论文对晚三叠世—中侏罗世早期盆地的形成与演化开展了研究,包括关键地层界面特征分析、关键地层时代归属分析、区域岩石地层、生物地层和年代地层的综合对比分析、区域沉积体系与沉积相分析、岩相古地理分析,最终建立晚三叠世—中侏罗世早期羌塘盆沉积—构造动力演化模式。1、系统的对各地层单元的界面分析发现:(1)肖茶卡组底界在盆地内部与中三叠统整合关系,在盆地北缘为沉积超覆于不同时代的前三叠系之上:(2)肖茶卡组顶界面发育古岩溶角砾岩,与上覆那底岗日组为岩溶不整合接触,说明肖茶卡组沉积时期的羌塘盆地是在早中三叠世的盆地基础发展起来的,后期出现了广泛的海退事件,使盆地结束沉积并遭受风化剥蚀作用;(3)中侏罗统雀莫错组的岩性组合特征、岩石化学特征、古生物化石混积和地层的沉积超覆现象均表现出裂陷环境下形成的伸展不整合面的特征。2、综合地层划分与对比分析认为:(1)肖茶卡组古生物化石组合反映其时代为晚三叠世卡尼期—若利期,根据其上被上三叠统那底岗日组不整合覆盖,将其时代厘定为卡尼期—若利期早期;(2)那底岗日组火山岩SHRIMP锆石U-Pb年龄在216~205 Ma之间,其时代主要为若利期,可能包含有瑞替期:(3)日干配错组底部火山岩的年龄、中上部化石组合及其被下侏罗统整合覆盖,综合反映的时代为晚三叠世若利期—瑞替期,而且那底岗日组火山岩和日干配错组火山岩的地球化学成分分析反映两者均为引张构造背景下的产物;土门地区的土门各拉组的下部岩性及界面特征、化石组合和上部可能被下侏罗统整合覆盖,综合反映其时代为若利期—若利期。

Basing on detailed field survey and laboratory researches on lithological features, mineralogical composition, geochemical and zircon SHRIMP U-Pb data, together with the mineralogical study of chromitite and mantle peridotite heavy mineral bulk sample, various proceedings and recognitions have been achieved:(1) The mantle peridotite is the remnants of partial melted MOR mantle altered by SSZ fluids.

通过详细的野外调查和室内岩石薄片的岩相学、矿物成分、岩石地球化学和锆石SHRIMP U-Pb同位素年代学,铬铁矿和地幔橄榄岩的人工重砂大样的矿物学研究,取得以下进展和认识:(1)认为康金拉地幔橄榄岩为部分熔融MOR地幔残余,叠加了SSZ流体的改造。

One is Phi Phi Don where several long white powdery beaches attract visitors here to sunbathe and swim, and the other is rocky Phi Phi Le where thousands of swifts nest inside the Viking Cave . With its emerald crystal sea, secluded beaches, wooded cliffed mountains, colourful coral reefs and undersea life, Phi Phi is a paradise in the Andaman.

一个是披披东岛 Phi Phi Don ,它有许多很长的白色粉状海滩,吸引无数游客到这里游泳,享受日光浴;另一个是披披雷岛 Phi Phi Le ,岛上尽是嶙峋的岩石岩石上有个海盗洞穴,洞内栖息着数以万计燕子,这些小燕子与披披岛的鲜绿色水晶海,幽静的海滩,树木繁茂悬崖峭壁山,五颜六色的珊瑚礁和海底世界形成一道天然风景线,简直就是安达曼人的天堂生活。

The granite body in the Jiangjunzhai tungsten deposit is a compound rockmass, which has the features of crust-derived type granite and is the product of comagmatic evolution.

岩石学和岩石地球化学研究表明,将军寨钨矿花岗岩体为一复式岩体,是同源岩浆演化的产物,具有壳源花岗岩的特征。

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