Based on the analysis on brachiopod fossils of the late middle Permian,the brachiopod extinction in Pre-Lopingian event of late middle Permian in this area can be divided into two sub screens: the first screen in the end of earlier Wushisanti Subage a...

通過川渝地區(qū)中二疊世晚期的腕足動(dòng)物化石資料的研究中文字幕高清一区二区三区，表明本地區(qū)中二疊世晚期的樂平世事件中腕足動(dòng)物的滅絕可劃分為前后2個(gè)不同的次級(jí)幕：早期的五十三梯亞期之末的第一幕和晚期的倒鉆巖亞期之末的第二幕人人操人人鲁操肉肉，且第二幕的滅絕規(guī)模要比第一幕更大。

Based on the analysis on brachiopod fossils of the late middle Permian, the brachiopod extinction in The Lopingian event of late middle Permian in this area can he divided into two sub screens: the first screen in the end of earlier Wushisanti Subage and the second screen in the end of later Daozuanyan Subage. The second screen's extinct scope is larger than the first screen's.

通過川渝地區(qū)中二疊世晚期的腕足動(dòng)物化石資料的研究WW亚洲天堂，表明本地區(qū)中二疊世晚期的樂平世事件中腕足動(dòng)物的滅絕可劃分為前后2個(gè)不同的次級(jí)幕：早期的五十三梯亞期之末的第一幕和晚期的倒鉆巖亞期之末的第二幕一级国产男女性爱带套午夜那些事，且第二幕的滅絕規(guī)模要比第一幕更大。

Castration+estrogenic hormones was used in 11 later prostate cancer patients, the effective rate was 81.9%, the recidivation rate was 44.4%, the average time of recidivation is 29.1 months.

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RESULTS : The hypertrophic cardiomyocyte NTPase Vmax values at 1 week group and 4 week group were all increased significantly in both of ATP and GTP as substrates with much higher argumental extent in early hyper group; their Km values were kept constant in early hyper group and were decreased only in late hyper groups.

結(jié)果：早、晚期肥大組心肌細(xì)胞核被膜NTPase最大反應(yīng)速率以ATP為底物時(shí)較對(duì)照組增加25%～62%(P＜0.01)，以GTP為底物時(shí)增加8%～44%(P＜0.01)久久久特级黄毛片免费看，其中晚期肥大組NTPase最大反應(yīng)速率增加幅度低于早期組欧美午夜艳。早期肥大組細(xì)胞核被膜NTPase Km值不變，晚期組NTPase Km值下降在线一区精品，以ATP和GTP為底物時(shí)晚期肥大組Km值分別下降22%和86%羞羞漫画免费观看网站。

As the results show: The two submerged macrophytes can also adapt to the polluted water. Under the condition of high nitrogen in the sediment, they can remove the nitrogen effectively, and the removal effect of Ceratophyllum demersum L.is better than Hydrilla verticillata Royle. Hydrilla verticillata Royle activates the TP in the sediment more effectively than Ceratophyllum demersum L.. The submerged macrophytes can intensify the removal effect of turbidity. But the CODMn removal effect of submerged macrophytes are not obvious.

結(jié)果表明：生長(zhǎng)晚期的黑藻和金魚藻仍可適應(yīng)污染河水；在底泥含氮量較高的情況下亚洲唯美国产区，生長(zhǎng)晚期的沉水植物對(duì)氮素具有明顯的去除效果久久自慰流水喷白浆免费看，且金魚藻的脫氮能力高于黑藻；黑藻對(duì)底泥中TP的活化能力高于金魚藻国产免费一级无码A；沉水植物可以強(qiáng)化濁度的凈化效果50岁熟女；沉水植物生長(zhǎng)晚期對(duì)CODMn的去除效果不高。

The Caledonian granitoids,majorly distributed in the northern Qimatage mountain,showing geochemical characteristics of Cordilleran I-type grantiods,low-K high-Ca amphibole-bearing calc-alkaline granitoids or peralkaline and alkaline granitoids,and associated with an active continental margin or back-arc basin,indicated the existence of the Qimatage ocean-related limited subdu...

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Increase of that clast of sedimentary rock, high-grade metamorphic rock and unstable heavy minerals shows tectonically active setting and obvious uplift of Bogda Mountain during the Late Jur.

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The differences in reservoiring conditions of natural gas and oil, as well as the multicycle developments and evolution histories of major gas bearing basins in China, and the geological environments characterized by relatively active tectonic movements in later period have resulted in the forming conditions of gas fields in China to be more complicated than those in many basins all over the world.

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We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry.(1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin.(2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively.(3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt.(4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau.(5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure.

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