Article said that China real estate exist "4" basin, the policy of "Basin"(negative profits, low tax, duty drawback, Blue India accounts Policy Focus), the interest rate "basin", taxation "Basin"(China not only low-tax and tax incomplete, no property tax, Trading income tax and inheritance tax, foreign Housing developed secondary trading value of the tax is generally 20% more serious bubble may upgrade to 50% or even higher, and some countries have also adopted a progressive tax to curb speculation) and the exchange rate "Basin"(short term appreciation of the existence of the Chinese exchange rate pressure, the international money watching), coupled with the love and structure of local government too low, leading to the coastal cities of residential living functional serious alienation and distortions residential speculation run wild.

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The basal geomorphology structure of the Tidal-Basin System of the Tiaozini Sandbanks is watershed and tidal creek system. We analyses its formation, evolvement, geomorphology characters and development and discusses the main influence factors which is water, sediment and space. We divide the evolution phases which is formation phase, autumn phase and contabescence phase. In the end we confirms its main functions, which is discharging the folium water on the tidal flat of the Tidal-Basin in the end of the ebb-tide, transporting sediment to Tidal-Basin through tidal creek systems, confining the swing range of the dynamical axis of flood tide or ebb tide, balancing the dynamical status of the South and North. At the same time, we compare coastal tidal-basin and sandbanks tidal-basin on geomorphology characters, formation causes, style and so on.

條子泥潮盆—潮溝系統(tǒng)的基本地貌結(jié)構(gòu)為分水灘脊和潮溝系統(tǒng)，本文分別對它們的形成與發(fā)育A一级毛片A一级黄片、地貌特點(diǎn)及動態(tài)變化進(jìn)行了分析久久免费影院，并探討了影響其發(fā)育的主要因素，即來水條件黄色稳定视频资源在线观看、來沙條件黄色免费a片短视频、空間條件，劃定了其主要發(fā)育階段日韩美女福利网址在线观看视频免费，即形成期欧洲激情一区二区三区视频、成熟期、衰亡期天天综合色一级毛片；在上述分析的基礎(chǔ)上確定了潮盆—潮溝系統(tǒng)的主要功能中文字幕网第一页，即通過潮溝系統(tǒng)渲泄落潮后期滯留在其潮盆范圍內(nèi)的灘面薄層水、通過潮溝系向潮盆內(nèi)部輸入或輸出泥沙色色色色色色色色色色色色色色色色色色色色、限制漲落潮動力主軸擺動范圍中文字幕日韩精品视频一区、平衡南北兩側(cè)動力狀態(tài)；同時(shí)針對岸灘潮盆—潮溝系統(tǒng)與沙洲潮盆—潮溝系統(tǒng)的地貌特征黄污视频免费网站、成因類型等進(jìn)行了對比分析激情图区自拍偷拍。

On basis of analysis of typical cases, four kinds of foreland basins were recognized:(1) subducted-collisional foreland basin;(2) retro-arc foreland basin (arc-continental collisional foreland basin);(3) intracontinental subducted foreland basin; and (4) strike-slip foreland basin.

在典型實(shí)例分析基礎(chǔ)上，劃分出四種類型的前陸盆地：(1)俯沖碰撞型前陸盆地超碰在线免费黄色；(2)弧后前陸盆地国产精品亚洲一级视频；(3)陸內(nèi)俯沖型前陸盆地；(4)走滑型前陸盆地黄页网站在线免费播放器。

Awati basin is an intracontinental forland basin in Cenozoic, which is different from peripheral foreland basin and retroarc foreland basin. It is a new kind of foreland basin caused by continental tectonic process.

新生代塔北阿瓦提前陸盆地為陸內(nèi)前陸盆地国产专区在线观看欧美狂野，是一種前陸盆地的新類型，即不同于周緣前陸盆地，也不同于弧后前陸盆地天天操天天怕天天日天天。

Three basin prototype s are generated in the southeast of Junggar Basin: filling basin in the post-rift sequenceP_2-T_(2-3,foredeep basin in the post-rift sequenceT~~3__3-J_(1-2 and intracontinental foreland basin(J_3-E).

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Based on the whole, dynamic and synthetical basin analytical methods, the structural characteristic of the South Ordos basin in the Late Mesozoic and the Cenozoic is researched with the data of seismic, geological and former achievements. In order to discuss deeply to the geodynamical background of Ordos basin and study the dominant factors controlling the sediment evolvement of the basin, we discusses the evolvement of basin from an even more extensive view.

采用&整體在线高清免费不卡无码黄片、動態(tài)中文字幕av有码高清片久久、綜合&的盆地分析方法，根據(jù)地震www.毛片基地、地質(zhì)等資料又粗又大又硬的黄片，結(jié)合野外地質(zhì)及前人研究成果，對鄂爾多斯盆地南部中-新生代以來后期改造特征進(jìn)行了研究日韩无码av毛片，深入探討控制鄂爾多斯盆地形成演化的地球動力學(xué)背景婷婷五月天视频，研究盆地構(gòu)造沉積演化的主控因素。

Based on the date of outcrop, log and lithology, sequence stratigraphic division and correlation were made on Neopaleozoic in south of North China Basin, and high-precision geologic correlation framework was built up in the basin.2. In the term of sedimentary features of Neopaleozoic in south of North China Basin, lateral variation of sedimentary facies was studied selectively in Benxi-Taiyuan Formation, Shanxi Formation, Lower Shihezi Formation, Upper Shihezi Formation and Shiqianfeng Formation. Lithofacies paleographic features and the sedimentary evolutionary process of Late Paleozoic in south of North China Basin were worked also.3. On the basis of sand-bodies Isopach figure drawing, the distribution of major reservoir sand-bodies of Neopaleozoic in south of North China Basin was studied. Basing on the distribution of sand-bodies in sequence stratigraphic framework, combining the development and distribution features of barrier and underwater distributary channel, there is a disquisition on the distribution regularity of pay reservoir sand-bodies of Neopaleozoic in this area.

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The basin experienced three basin-forming cycles of Neopaleozoic, Mesozoic and Cenozoic Eras. Mesozoic fault and depression compounding basin composed the northern margin Jurassic petroleum system and the Cenozoic large-scale strike-slip and compressional basins composed the Tertiary petroleum system of the western Qaidam basin and Quaternary petroleum system of Sanhu. The intense tectogenesis of Yanshan and Xishan made the Jurassic petroleum system of the northern Qaidam more complex. The monocycle paleoclimate evolution in Cenozoic Era and multi-tectonic movement made the lake-basin evolution, hydrocarbon source-rock, reservoir development, accumulation condition and petroleum distribution are more exceptive in character and complex in feature.

該盆地經(jīng)歷了晚古生代2019人人操人人摸、中生代和新生代3個(gè)成盆旋回，中生代斷坳復(fù)合盆地形成了柴達(dá)木盆地北緣侏羅系油氣系統(tǒng)免费关看黄色视频，新生代大型走滑擠壓盆地形成了柴達(dá)木盆地西部第三系油氣系統(tǒng)和三湖第四系天然氣系統(tǒng)日本黄色网站大全，燕山和喜山2期強(qiáng)烈構(gòu)造運(yùn)動使柴北緣侏羅系油氣系統(tǒng)高度復(fù)雜化，新生代單旋回古氣候演化與多期構(gòu)造運(yùn)動使湖盆演化性交BBW、烴源巖和沉積儲層發(fā)育特征本页影院、成藏條件與油氣分布規(guī)律變得十分特殊和復(fù)雜。

From the research of the kerogen carbon isotopes of the coal-measure strata in some basins of China (the Carbo-Permian in the Ordos basin, the Triassic in the Sichuan basin, the Jurassic in the Jungar basin and Turpan-Hami basin, the Tertiary in the Yingqong basin) it can be indicated that the Type Ⅲ kerogen has a wide δ〓C range from -21. 2‰ to -27. 6‰, averaging -25‰, which is more enriched in 〓C than sapropel and mixed kerogens.

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When one basin changed from rifting basin to foreland basin, it presents different stages of basin evolvement in time series, and presents different basin types in special series.

從裂陷盆地向前陸盆地的轉(zhuǎn)化過程中国产成人在线无码视频，在時(shí)間序列上表現(xiàn)為盆地演化階段的不同富婆按摩高潮对白在线观看，在空間序列上表現(xiàn)為盆地類型的不同。