And now that thou art lying, my dear old Carian guest

如今，你的藝術(shù)依舊国产精品久久久精品日日，我親愛的卡里亞的老貴賓

And now that thou art lying, my dear old Carian guest

如今欧美黄色网站的网址，你靜臥著，我親愛的卡里亞的老貴賓

And now that thou art lying, my dear old Carian guest

一把灰白的骨殖6080无码吃奶在线观看视频，很久很久前就已經(jīng)安息

He employed Greek and Carian mercenaries and encouraged Greek traders to establish a few Greek towns in Egypt.

他組建了由希臘和迦南人構(gòu)成的雇傭軍操av在线，鼓勵(lì)希臘商人在埃及建立了許多希臘人的城鎮(zhèn)。

During early middle Jurassic period, Quemocuo formation in NQB was offshore lake deposition with marine feature, in SQB was shelf deposition, which indicted that an intense rifting and sea level rising with more large range, and consequently, eroding area was shrunk and deposition area was expanded.4. According to the result of stratigraphic surface features, division and correlation, and the paleographic characteristic, Qiangtang Basin during late Triassic -early middle Jurassic period could be divided into two basin developing stages with difficult tectonic nature, remnent epicontinental basin stage in Carian -early Norian of late Triassic and rifting basin stage in middle Norian of late Triassic - early middle Jurassic period respectively.

雀莫錯(cuò)組在羌北盆地為近海湖泊沉積你懂得黄色网址，更具海相色彩：南羌塘主要為外陸棚沉積久久强奸中文视频，反映羌塘盆地再次發(fā)生較強(qiáng)烈的裂陷作用和較大幅度的海平面上升，形成陸源剝蝕區(qū)縮小亚洲精品在线小视频，沉積覆蓋面增大的古地理面貌色色色色色色色色7。4、根據(jù)地層界面特征一本无码字幕在线少妇人妻、地層劃分與對(duì)比結(jié)果和巖相古地理演化特征可將晚三疊世—中侏羅世早期羌塘盆地劃分為兩個(gè)不同構(gòu)造性質(zhì)的盆地發(fā)展時(shí)期日韩精品不卡一区2区，分別為晚三疊世卡尼期—若利早期的殘留內(nèi)陸表海沉積盆地發(fā)展與消亡時(shí)期和晚三疊世若利期中晚期—中侏羅世早期的裂陷盆地的形成與發(fā)展時(shí)期。

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.

論文對(duì)晚三疊世—中侏羅世早期盆地的形成與演化開展了研究天天欧美色干，包括關(guān)鍵地層界面特征分析国产综合在线视频、關(guān)鍵地層時(shí)代歸屬分析、區(qū)域巖石地層欧洲熟妇色XXXX欧美老妇、生物地層和年代地層的綜合對(duì)比分析欧美黄色小视频免费观看、區(qū)域沉積體系與沉積相分析、巖相古地理分析人人操人人狠，最終建立晚三疊世—中侏羅世早期羌塘盆沉積—構(gòu)造動(dòng)力演化模式丰满熟妇口爆吞精。1、系統(tǒng)的對(duì)各地層單元的界面分析發(fā)現(xiàn)：(1)肖茶卡組底界在盆地內(nèi)部與中三疊統(tǒng)整合關(guān)系亚洲一区黄片，在盆地北緣為沉積超覆于不同時(shí)代的前三疊系之上：(2)肖茶卡組頂界面發(fā)育古巖溶角礫巖www.久久思思热.com，與上覆那底崗日組為巖溶不整合接觸，說明肖茶卡組沉積時(shí)期的羌塘盆地是在早中三疊世的盆地基礎(chǔ)發(fā)展起來的黑人与黑人作爱A级毛片，后期出現(xiàn)了廣泛的海退事件老熟妇一区二区免费视频，使盆地結(jié)束沉積并遭受風(fēng)化剝蝕作用；(3)中侏羅統(tǒng)雀莫錯(cuò)組的巖性組合特征人妻欧美精品片在线97、巖石化學(xué)特征www。五月天。com、古生物化石混積和地層的沉積超覆現(xiàn)象均表現(xiàn)出裂陷環(huán)境下形成的伸展不整合面的特征。2国内免费的黄色视频在线观看、綜合地層劃分與對(duì)比分析認(rèn)為：(1)肖茶卡組古生物化石組合反映其時(shí)代為晚三疊世卡尼期—若利期全网最新黄色网站，根據(jù)其上被上三疊統(tǒng)那底崗日組不整合覆蓋，將其時(shí)代厘定為卡尼期—若利期早期一级在线播放；(2)那底崗日組火山巖SHRIMP鋯石U-Pb年齡在216～205 Ma之間久久久极品精品，其時(shí)代主要為若利期，可能包含有瑞替期：(3)日干配錯(cuò)組底部火山巖的年齡www.99re6.com、中上部化石組合及其被下侏羅統(tǒng)整合覆蓋偷拍自慰，綜合反映的時(shí)代為晚三疊世若利期—瑞替期，而且那底崗日組火山巖和日干配錯(cuò)組火山巖的地球化學(xué)成分分析反映兩者均為引張構(gòu)造背景下的產(chǎn)物人人操操草草；土門地區(qū)的土門各拉組的下部巖性及界面特征日韩黄色片网站、化石組合和上部可能被下侏羅統(tǒng)整合覆蓋，綜合反映其時(shí)代為若利期—若利期黄色视频一级片免费。

He made himself master of what is now called the Hellenic sea, and ruled over the Cyclades, into most of which he sent the first colonies, expelling the Carians and appointing his own sons governors; and thus did his best to put down piracy in those waters, a necessary step to secure the revenues for his own use.

他使自己成為現(xiàn)在的希臘海的霸主那里能看免费毛片，對(duì)Cyclades制定法規(guī)，在那里他最早建立了殖民地欧美黃色网络，驅(qū)逐了Carian人无码作爱高潮视频，任命他的兒子為統(tǒng)治者；全力鎮(zhèn)壓該水域的海盜欧洲aaaa片，作為保護(hù)他自己的稅收的一個(gè)必要措施强奸乱伦国产精品字幕。