First,we have discovered stone artefacts in caves, which have similar features to that were broadly scattered in laterite terraces in Bose basin(0.8 Ma B.P),next study on deposits and fauna will be hopefully contributed to document paleoenvironmental background of early human;Second,early human fossils,Gigantopithecus and mammalian fossils unearthed in Mohui cave provide new evidence of early human origin; Third,after our scientific excavation in Fengshudao site in Bose basin, we have found five pieces of bi-face LCT with 10 tektites and nearly 100 stone artefacts form original laterite deposit.This important discovery is very answerable to international question about stratigraphic suspect of LCT; Fourth, abounding mammallian fossils with human fossils and remains from early Pleistocene to Holocene have been uncovered after systematically excavation in marginal cave of Bose basin.These discoveries are significant to the study on human evolution and establishment of sequence of Quarternary biological-stratigraphic in southern China.

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The lithologic pool such as that developed in the actic region while the basin is rifting or in the glacis region while the basin is depressing all which can be found in this basin. Five kinds of sedimentary facies and thirteen sedimentary parfacies can be found in the Shengbei concave during the period of Jurassic series and Cretaceous series.

在該盆地內(nèi)部既有可能發(fā)育斷陷期陡坡帶的巖性油氣藏国际a极性爱片，又有可能發(fā)育坳陷期緩坡帶的巖性油氣藏91小黄片，其勝北洼陷在中侏羅統(tǒng)－白堊系沉積時期主要發(fā)育5種陸相沉積相類型、10種沉積亞相類型全网高清国产AV网站。

The Turpan Basin is an intermountain basin in the Tianshan Mountains. A good preservation of the Paleogene in this basin provides abundant information for studying of the Paleogene climate in Northwest China.

吐魯番盆地是天山山脈中的一個山間盆地插入美女国产，古近系保存完好，是研究中國西北地區(qū)古近紀(jì)氣候變遷的良好地區(qū)小草在线免费观看av。

Main differences between intracontinental foreland basin and typical foreland basin have been analyzed and main sedimentary characteristics of the intracontinental foreland basin have been proposed.

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The Kuche Basin, located between the Tianshan intracontinental orogenic belt and the Tarim plate, Xinjiang Uygur Autonomous Region, northwest China, is the tectonic element in the Mesozoic-Cenozoic time, and belongs to a new type of intracontinental flexural basin in the classification of the basin.

庫車盆地位于天山陸內(nèi)造山帶與塔里木板塊之間，是中新生代發(fā)育的構(gòu)造單元，在盆地分類上屬于一種新的陸內(nèi)撓曲盆地黄色网页视频久久。

Foreland basin is mainly located in the frontier of the thrust faulting of orogenic belt while the intracontinental basin is situated in the inland area of the basin.

準(zhǔn)噶爾盆地是多期構(gòu)造擠壓環(huán)境下演化形成的大型陸內(nèi)疊合盆地亚洲美女4p变态网站，其盆地類型既有前陸盆地，也有陸內(nèi)凹陷欧美亲近乱子伦电影，其中在线h精品，前陸盆地主要分布在造山帶逆沖斷裂前緣，陸內(nèi)凹陷主要分布于盆地內(nèi)陸區(qū)色播播影院,噜噜噜噜私人影院。

Tectonic evolution of Lanping basin, controlled by closure of Palaeo-Tethys and collisional orogen between India plate and Asia continent, has undergone three evolutional stages, i. e., intracontinental rift, sag basin and strike-slip basin.

蘭坪盆地的構(gòu)造演化受控於古特提斯的閉合及印度與亞洲大陸碰撞的造山作用，盆地經(jīng)歷了陸內(nèi)裂谷人人干人人插日日操、拗陷盆地和走滑盆地3個階段的發(fā)育過程。

Main recognition bases of the Gangdisê multiple island arc-basin system are:① tectonic pattern of collisional zones and island arc or landmass as strips alternating with blocks;②development of multiple arc volcanic-intrusive zones due to consumption of back-arc basin and arc-arc collision;③complicated paleogeographic and paleotectonic patterns shown by numerous sedimentary basin types and sedimentary facies association.

岡底斯構(gòu)造帶多島弧—盆系統(tǒng)識別的主要依據(jù)有：①構(gòu)造帶中發(fā)育碰撞結(jié)合帶與島弧或陸塊呈條塊相間的大地構(gòu)造基本格局亚洲色图综合区；②發(fā)育多條由弧后盆地衰亡和弧—弧碰撞作用而形成的弧火山—侵入巖帶；③眾多的沉積盆地類型和沉積相組合欧美日韩国产在线一区，反映出岡底斯構(gòu)造帶具有復(fù)雜的古地理和古構(gòu)造格局。

Qaidam basin is located in north of Qinghai province, and it is a large Mesozoicand Cenozoic oleaginous basin ,the total acreage is about 12×104km2. Sanhu regionin east of Qaidam basin is explored and founded the Quaternary biogas, the thicknessof Quaternary strata is 3200m;the diagenesis is in low degree, high porosity and highpermeability;the sand and mud are interbeddings, sand is reservior and mud is gassource rock and cover rock;stock size of Quaternary biogas achieve 12476×108m3 ,the explored geological reserve is 1472×108m3, the third class reserve is about 3500×108m3. It is the region where founded the largest scale of biogas in the world.

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