The source rocks of the former are mainly the well-developed, huge thickness of Neogene marine depression sedimentary rocks and Miocene marine sedimentary rocks; those of the latter are significantly the rift sediments of Paleogene continental facies, and large-scale source rocks of medium-deep lacustrine facies and inshore paludal facies with coal measure strata well-developed.

根據(jù)南海北部邊緣新生代沉積盆地結(jié)構(gòu)乱弄欧美丰满胖老熟妇、構(gòu)造特征可將其劃分為走滑伸展型和斷陷裂谷兩大類型，前者以新近系巨厚海相坳陷沉積及海相中新統(tǒng)烴源巖發(fā)育為突出特點(diǎn)，后者則以古近系陸相斷陷裂谷沉積和大規(guī)模中深湖相烴源巖、近海沼澤相煤系烴源巖發(fā)育為主要特征精品视频只有这里有，這些烴源巖的發(fā)育展布規(guī)律、有機(jī)質(zhì)豐度和生烴母質(zhì)類型色综合影院网、成熟演化特點(diǎn)以及生烴潛力等均差異較大久久精品国产99精品九九。

The tectonic evolution history of Tianshan is an example. In the Triassic, it was once uplifted to form the mountains with thick molasse accumulation on both its sides, Junggar and Tarim Basins. Then it became a peneplain by the exposion and deplanation in the Jurassic, forming the widespread coal-bearing strata which can be correlated. From the Cretaceous to the Early Cenozoic, it was uplifted again, until the Quaternary to build huge mountains with two large sedimentary basins on both sides.

如天山山脈的構(gòu)造演化，三疊紀(jì)天山曾經(jīng)一度隆起成山av中字在线网站，兩側(cè)的準(zhǔn)噶爾和塔里木盆地中堆積了巨厚的磨拉石99热嫖妓国语对白；侏羅紀(jì)時(shí)由於剝蝕夷平成為一個(gè)準(zhǔn)平原，形成了廣泛分布且可以對(duì)比的含煤巖系成人在线观看网站；從白堊紀(jì)到早新生代www日韩视频，它再度隆升，直至第四紀(jì)時(shí)形成雄偉的高大山系欧美日韩国产精品，兩側(cè)形成相應(yīng)的大型沈積盆地99在精品。

Attend a news briefing once personate " mad stone " in " path elder brother " Liu Hua and personate " black skin " Huang Bo, hao of Yu of Neozoic high grade God bright, 3 actor also are conduct propaganda of this MSN brand piece main actor.

出席發(fā)布會(huì)的曾經(jīng)飾演《瘋狂的石頭》中"道哥"的劉樺和飾演"黑皮"的黃渤，新生代優(yōu)質(zhì)偶像俞灝明国产精品人爱超碰资源，三位藝人也是此次MSN品牌宣傳片的主演亚洲一区二区三区久久精品视频。

In some cases, stratigraphic relations require these excursions to be sustained for millions of years at values even below the mantle average of -5‰, the minimum value for a steady state C isotope mass balance in the Phanerozoic ocean.

某種程度上來說，層序的相關(guān)性需要至少低于地幔平均值-5‰并且至少多個(gè)百萬年的同位素?cái)?shù)值來獲得美女网站视频免费黄国产，穩(wěn)定碳同位素最小值對(duì)于新生代海洋碳同位素平衡起到了平衡的作用。

According to drilling, logging and seismic data in the north of the basin, four types of identification signs were determined to the Phanerozoic sequence boundary. And two kinds of sequence boundaries (unconformity and shift surface of deposition) were identified.

應(yīng)用層序地層學(xué)的原理和方法精品区二区三区免费A片视频，綜合研究盆地北部鉆井免费黄色网站视频亚洲、測(cè)井及地震資料，確定4種層序界面識(shí)別標(biāo)志国产乱子论在线一区二区视频，在盆地北部新生代始新世—中新世識(shí)別出2種類型層序界面：不整合面和沉積作用轉(zhuǎn)換面www..com5566品久久99。

Based on the dating of Late Cenozoic strata and lithology changes analyses, it can infer the ages of layer landforms formation and the time of broken planation surface.

通過對(duì)晚新生代沉積地層高分辨率的環(huán)境磁學(xué)研究可進(jìn)一步捕捉重大的環(huán)境變化事件，測(cè)定其形成的年代及變化欧美一级欧美一级A片，并推測(cè)剝蝕面形成和抬升的時(shí)間以及確定這些層狀地貌形成的時(shí)代黄色视频在线观看com，進(jìn)而推演六盤山和青藏高原構(gòu)造隆升的歷史。

This is Lynda La Plante at her best, creating a compelling, charismatic new detective in Anna Travis, and bringing to vivid life on the page a completely gripping crime thriller

這是Lynda La Plante的顛峰之作，她把安娜˙翠薇思刻畫成了一位魅力無窮的新生代警探欧美性爱视频一区在线观看，也為我們呈現(xiàn)出了一部扣人心弦的犯罪驚悚作品女生奶头视频。

Environmental changes and it's responding to tectonic uplift of Tibetan Plateau are summarized in this article.

青藏高原的形成是新生代地球歷史上最重大的地質(zhì)事件之一。

By study of the medium-acid plutonic rock and its maric microgranular enclaves of the middle Gangdis〓 belt, this dissertation will discuss the characteristics of the Gangdis〓 medium-acid plutonie magmatism and the crust/mantle dynamics during uplifting of Tibetan Plateau from the sight of material and energy, and use'lithoprobe'to connect crust and mantle interaction and other geologic events.

中孕妇三级片在线观看、新生代青藏高原巖漿活動(dòng)強(qiáng)烈A级毛片中文字幕完整版，沿雅魯藏布江縫合帶形成了著名的岡底斯構(gòu)造—巖漿帶，本篇博士論文以岡底斯帶中酸性侵入巖及其中鐵鎂質(zhì)微粒包體為研究重點(diǎn)欧美激情2，探討岡底斯帶中酸性侵入巖漿活動(dòng)特征黄色网站视频你懂得，從物質(zhì)和能量的角度論述了高原隆升過程中的殼/幔動(dòng)力學(xué)過程，利用"巖石探針"將殼/幔之間的相互作用和地質(zhì)事件有機(jī)地結(jié)合起來苍井空全集百度影音。

Four stages of granitoid plutonism took place in Precambrian, early Paleozoic （∈-D3）, late Paleozoic-early Mesozoic （D3-T3）, and late Mesozoic-Cenozoic, respectively.

該帶內(nèi)的花崗巖形成可以劃分為4個(gè)時(shí)段毛片国产一国产AN毛片，分別與4個(gè)造山旋回相對(duì)應(yīng)：前寒武紀(jì)；早古生代日韩高清第一页；晚古生代—早中生代性色av无码一区二区；晚中生代—新生代。