The system consists of the following procedure: pre-concentration of metallogenic matter in living organisms in primary depositional basin; solution, absorption and concentration of metallogenic matter in organic matter and organic thermal fluid generated from organisms during lithogenesis; migration of metallogenic matter in organic thermal fluid from basin to mountain region and activation of metallogenic elements by organic matter and organic thermal fluids in sedimentary strata in mountain regions during basin compaction and mountain building; metallization due to reactions between inorganic fluid and organic fluid bearing metallogenic matter and because of reductions and absorptions by organic matter in mountain regions.

生物成礦系統(tǒng)的內(nèi)容是：在原始盆地接受沉積時(shí)毛片网站在线播放，生物對金屬成礦物質(zhì)就存在預(yù)富集作用国内久久久久久精品影片；在成巖過程中国内99在线，生物轉(zhuǎn)化為有機(jī)質(zhì)及有機(jī)熱流體国产黄色视频观看，對金屬成礦物質(zhì)存在溶解日欧美老女人、萃取、富集作用日本在线欧美在线；在盆地壓實(shí)和造山活動中韩国一级婬乱片高清视频一，盆地中有機(jī)熱流體向造山帶運(yùn)移，此過程流體攜帶大量成礦物質(zhì)欧美性爱网址，對金屬成礦物質(zhì)存在遷移作用女被男c网站，而處于造山帶沉積地層中的有機(jī)物及有機(jī)流體對金屬成礦元素存在活化作用；盆地有機(jī)熱流體與造山帶含金屬流體會合另类综合80P，以及造山帶有機(jī)質(zhì)及有機(jī)流體對金屬元素進(jìn)行還原和吸咐美女汚汚无遮挡免费视频，最終形成金屬礦床，對金屬成礦物質(zhì)存在成礦作用欧美日韩国产手机在线观看视频。

The biometallogenesis system of Jinya gold deposits consists of the following procedure: pre-concentration of gold and metallogenic matter in living organisms in Luodian-Danchi rift depositional basin; solution, absorption and concentration of metallogenic matter in organic matter and organic thermal fluid generated from organisms during lithogenesis; migration of gold and metallogenic matter in organic fluid from basin to Lingyun underwater carbonate platform and concentration at its boundary convex (palaeo-blind-mountain) during basin compaction ; metallization due to depth thermal fluid making organic fluid thermal degradation and forming new fluid which riches in gold and sulfur, and the fluid migrating upward and depositing in upside ore-controlling structures because of absorptions by organic carbon and atc.

通過研究金牙金礦作用的生物成礦系統(tǒng)內(nèi)容為：在早日本超碰97人人爽人人爱、中三疊世羅甸—丹池裂谷盆地接受沉積時(shí)，生物對金等成礦物質(zhì)就存在預(yù)富集作用操操av网；在成巖過程中igao.com视频在线，生物轉(zhuǎn)化為有機(jī)質(zhì)及有機(jī)熱流體，對生物及沉積物中的金等成礦物質(zhì)存在溶解免费va欧美高清不卡一区在线、萃取日韩欧美亚洲中文字幕看、富集作用色色色。com；在盆地壓實(shí)成巖作用中，盆地中有機(jī)熱流體向凌云水下碳酸鹽臺地運(yùn)移农村女人一级毛片20岁的毛片，并在臺地邊緣外凸部位集中老王黄色网站中文字幕，此過程流體攜帶大量成礦物質(zhì)，對金等成礦物質(zhì)存在遷移集中作用性爱激情小说视频；深部熱流上侵使有機(jī)流體發(fā)生降解和釋放金的熱作用97人伦人妻对对碰免费看、形成高含金的有機(jī)熱液，含金熱液上移在構(gòu)造通道中沉積并被有機(jī)碳再次吸附三级片免费观看视频，最終形成金礦床91精品免费一区二区三区，對金存在成礦作用。

As a fault basin, Jiyang depression experienced multicycle evolvements, and the developing characteristics of the faults in each structural stage controlled not only the prototype basin pattern, but also the denudation and alteration of the previous basin.

作為斷陷盆地午夜摸一摸A片，濟(jì)陽坳陷自中生代以來亚洲免费的中文小说图片，經(jīng)歷了多期次的盆地演化過程，各時(shí)期的斷裂發(fā)育特征不僅控制了當(dāng)時(shí)的原型盆地格局欧美一级日逼视频，也主導(dǎo)著對先期盆地的剝蝕改造美女自慰喷水黄色网站，盆地的疊合關(guān)系直接控制了殘留盆地格局。

Recently, the discovery of different kinds of commercial hydrocarbon flow in Neopaleozoic of Ordos Basin, Jizhong and Huanghua depression in Bohai Bay Basin, and Qinshui Basin has indicated that Neopaleozoic is a subject reservoir with broad prospect in North China.

近期三级黄视频一区二区三，鄂爾多斯盆地黄色网站视频污污污黄色、渤海灣盆地的冀中及黃驊坳陷和華北沁水盆地的上古生界都已獲得了規(guī)模不等的工業(yè)油氣流，顯示華北地區(qū)的上古生界是一套極具勘探前景的目的層系亚洲性爱区第一页。

And combined with the transformation of the basin-basin and basin-mountain formed by Caledonian movement, the author thinks that,(1)the Yangtze and Huaxia are still the different plates in Caledonian period, Yangtze plate is subduction plate, Huaxia plate is obduction plate by the activation of PreSinian period tectonic plate joint belt.

首先欧美男女性潮免费福利看，雖然有古地磁資料表明兩地塊從震旦紀(jì)到奧陶紀(jì)是逐漸靠攏并拼接在一起的，但華南地區(qū)至今沒有找到證實(shí)這次碰撞結(jié)合的含有加里東洋殼殘片在內(nèi)的蛇綠巖混雜帶人人看人人看，也沒有發(fā)現(xiàn)與之有關(guān)的溝弧盆體系青青青手机视频在线，對此有著不同的解釋，這也是研究區(qū)多年來一直困擾許多地質(zhì)學(xué)家的原因在线观看免费黄色网站，也是大家一直爭論的熱點(diǎn)欧美性视品。

During the sediment of late Cretaceous Taizhou Formation and Paleocene Epoch Funing Formation, Subei Basin have formed dark shale containing lots of ostracoda that include predominated whole basin E12 Formation and E14 Formation and local K2t2 Formation, which have become main source rocks of the basin.

海侵的原因，可能是從晚白堊世晚期起黄色网站免费看a片，中國東部的地應(yīng)力條件以引張力占優(yōu)勢作爱免费视频网站，并在華北－渤海灣、蘇北－南黃海和東海陸架區(qū)欧美性爱αV在线视频，發(fā)育了一系列為早第三紀(jì)巨厚沉積物所充填的半地塹箕狀盆地欧美精品性，海水由東海向黃海海侵，造成陸架上箕狀盆地在短時(shí)期內(nèi)與海水相通在线观看黄A片免费网站AI换你。

Integrated analysis based on stratigraphy, sedimentary facies and paleophysiography data indicate that small basin-mountain pairs formed in the Kuche Basin during early Mesozonic, and large basin-mountain pairs.

地層又刺激又黄色网站、沉積相，生物古地理等綜合分析表明庫車盆地中生代早期形成了小波長盆山共軛對，中晚期為大波長盆山對久久精品国产高潮AV。

Directed under plate tectonics theories, author applied the relationship between orogenyy belt and basin, analyzation of proto-type basin restoration of Paleo-structures etc to systematically draw the Paleo-structural maps and Paleo-sedimental photographical maps on Z, O, S, D, C, P, T, J, K, E, N〓j, N1〓k, N〓k etc in Tarim basin.

以板塊構(gòu)造理論為指導(dǎo)在线黄网站，運(yùn)用造山帶與盆地、原型盆地分析黑人AAAAAAAA片免费、古構(gòu)造分析等分析方法91精品人妻综合导航，系統(tǒng)編制了Z、O18禁午夜老色批福利院、S成年人的免费在线视频、D、C国产在线精选、P永久免费黄色毛片、T日韩一级欧美一级二级在线观看视频、J欧美一A片网站、K、E轮奸网站、N〓j国产精品免费观看26uuu、N〓K，N〓K等盆地及周緣古構(gòu)造巖相圖久草久草久草，全面系統(tǒng)地研究和恢復(fù)了塔里木大型疊合復(fù)合盆地構(gòu)造演化歷史亚洲啪啪黄片，并將塔里木盆地構(gòu)造演化史劃分為7個(gè)構(gòu)造演化階段。

In Chapter 4, using the points of view of dissipative theory, the dissipative structure characteristics of ecological-economic system in the Changjiang River basin is analyzed, the development course and evolution characteristic of the ecological-economic system in the Changjiang River basin is demonstrated, and at last the negentropy sources and the entropy value of the ecological-economic system in the Changjiang River basin is radicated.

第四章運(yùn)用耗散結(jié)構(gòu)觀分析研究了長江流域生態(tài)經(jīng)濟(jì)系統(tǒng)耗散結(jié)構(gòu)特征日韩伊人自拍视频网站在线，并用耗散結(jié)構(gòu)理論論證了長江流域生態(tài)經(jīng)濟(jì)系統(tǒng)演變過程與演化特征国产浓毛熟女免费视频，最后確立了長江流域生態(tài)經(jīng)濟(jì)系統(tǒng)的負(fù)熵源與熵值。

Analysis on mineral characteristics (percent of shingly fragment, maturation index and heavy mineral coefficient of stability) and depositional environment in Mesozoic remanet strata show that provenance located in the north of Yanqi basin, clast were moved from north to south in Mesozoic, and the sedimentary environment in northern basin were braided stream facies while shallow lacustrine stream facies in southern basin.

通過對焉耆盆地現(xiàn)今殘留中生代地層中的巖礦特征(碎屑含礫百分比2019av亚洲天堂、成熟度指數(shù)和重礦物穩(wěn)定系數(shù))及沉積環(huán)境分析A片三集片在线hu免费，焉耆盆地中生代物源區(qū)位于盆地北部，碎屑由北至南搬運(yùn)av网站直接看；盆地北部為辮狀河相沉積環(huán)境毛片视频免费看，南部為淺湖相沉積環(huán)境。