core complex造句
例句與造句
- metamorphic core complex; ag-au deposit; geological and geochemical characteristics; eastern hebei
變質(zhì)核雜巖銀金礦床地質(zhì)地球化學(xué)冀東 - aim in order to determine whether the metamorphic complex of xiaoqinling area is metamorphic core complex or not
摘要目的為確定小秦嶺地區(qū)發(fā)育的變質(zhì)雜巖體是否屬于變質(zhì)核雜巖。 - the geological and geochemical characteristics of ag-au mineral deposits related to the metamorphic core complexes in the eastern hebei
冀東變質(zhì)核雜巖中銀金礦床地質(zhì)地球化學(xué)特征肖成東 - the matching connection between the effective hydrocarbon source rock in jurassic and the other factors of formating-resource in kuche is also influenced by the time of formation of the metamorphic core complex
同時還認(rèn)為變質(zhì)核雜巖的形成時期還影響了庫車坳陷侏羅系主力烴源巖同其他成藏要素的匹配關(guān)系。 - the small subcomlexes composed of elp4 / 5 / 6 is required for the hat activity, it interacts preferentially with the core complex ( rather than in complex with rnapii ) and was therefore proposed to have a regulatory function
復(fù)合物的hat活性需要elp456的存在，它們只與核心復(fù)合物相互作用(不與rnap作用)，可能對核心復(fù)合物的hat活性具調(diào)控作用。 - It's difficult to find core complex in a sentence. 用core complex造句挺難的
- oxygen-evolving psil core complexes treated with hydrophilic crosslinker edc showed a little change in the microenvironments of tyr and trp residues . however, oxygen-evolving psil core complexes treated with hydrophobic crosslinkers such as dcc, hmdi, egs, and dtsp showed a distinctly change in both the microenv
egs、dtsp對psll放氧核心復(fù)合物蛋白質(zhì)中tyr、trp微環(huán)境和682urn處葉綠素?zé)晒庥绊懘?，可能它們參與了psll放氧核心復(fù)合物內(nèi)部的蛋白疏水區(qū)域交聯(lián)。 - oxygen-evolving psil core complexes treated with hydrophilic crosslinker edc showed a little change in the microenvironments of tyr and trp residues . however, oxygen-evolving psil core complexes treated with hydrophobic crosslinkers such as dcc, hmdi, egs, and dtsp showed a distinctly change in both the microenv
egs、dtsp對psll放氧核心復(fù)合物蛋白質(zhì)中tyr、trp微環(huán)境和682urn處葉綠素?zé)晒庥绊懘螅赡芩鼈儏⑴c了psll放氧核心復(fù)合物內(nèi)部的蛋白疏水區(qū)域交聯(lián)。 - the ps ii native fractions ( 20 % and 30 % ) were loaded onto a deae column . the fraction eluted with 150 mm nacl was presented dcip reduction activity and was highly depleted in chi c and xanthophylls, and as such could be considered a ps ii core complex
對于有dcip光還原活性的20和30層帶的復(fù)合物，進一步deae離子交換層析純化。150mmnacl洗脫純化后的樣品經(jīng)過熒光激發(fā)光譜測定發(fā)現(xiàn)，已經(jīng)去除了葉綠素c和墨角藻黃素，并且仍然具有dcip的光活性，分析是ps核心復(fù)合物。 - yeast elongator was isolated as a complex that associates with the chromatin fraction and interacts with the elongating phosphorylated form of rnap ii . the functional entity of elongator complex has recently been shown to be an unstable six-subunit complex, termed holo-elongator, which can dissociate into two discrete three-subunit subcomplexes upon treatment with high salt and / or monoq chromatography . one of these subcompexes is the elp3-containing core complex, and the other is a complex of the elp4, elp5 and elp6 proteins
酵母elongator是與染色質(zhì)組分結(jié)合，并與延伸中的磷酸化形式的rnap相互作用的復(fù)合物，是個六亞基的功能整體，在高鹽處理或monoq層析時易于分解為兩個三亞基亞復(fù)合物，其中一個是含elp3的核心復(fù)合物，另一個含elp456亞基。 - yinggete-bagemaode metamorphic core complex belt with three-layer construction is put forward, which evolved from late jurassic to cretaceous . the extensional simple shear model of the chagan fault depression is established . the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic-cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure
討論了查干凹陷及鄰區(qū)中-新生代盆地構(gòu)造演化及其地球動力學(xué)特征，三疊紀(jì)(印支期)為陸內(nèi)造山作用與地殼增厚、隆升剝蝕階段；侏羅紀(jì)(燕山早期)為造山后造山帶的局部伸展垮塌階段；白堊紀(jì)(燕山晚期)為造山期后大規(guī)模伸展垮塌作用與伸展盆地的發(fā)育階段；新生代(喜山期)為遠距離碰撞效應(yīng)與弱擠壓撓曲性質(zhì)的穩(wěn)定大陸內(nèi)坳陷的發(fā)育階段。 - to detect whether crosslinking reaction influence the fluorescence properties of the samples, oxygen-evolving psil core complexes were treated with five crosslinking agents at different concentration, then the chlorophyll fluorescence emission, excitation, and intrinsic fluorescence spectra of these samples were measured . the results showed that both chlorophyll fluorescence and intrinsic fluorescence of oxygen-evolving psil core complexes were altered by the crosslinking reaction . the maximum chlorophyll fluorescence band at 682 nm decreased and the intrinsic fluorescence emission intensity at 308 nm and 328 nm either increased or decreased
結(jié)果表明：交聯(lián)處理對psll放氧核心復(fù)合物葉綠素?zé)晒夂蛢?nèi)源熒光都有影響，引起682urn處葉綠素?zé)晒鈴姸鹊慕档汀?08urn或328urn處蛋白質(zhì)內(nèi)源熒光強度的增大或減小，并與處理時所用交聯(lián)劑的濃度、交聯(lián)劑的親疏水性和交聯(lián)臂長相關(guān)。 - to detect whether crosslinking reaction influence the fluorescence properties of the samples, oxygen-evolving psil core complexes were treated with five crosslinking agents at different concentration, then the chlorophyll fluorescence emission, excitation, and intrinsic fluorescence spectra of these samples were measured . the results showed that both chlorophyll fluorescence and intrinsic fluorescence of oxygen-evolving psil core complexes were altered by the crosslinking reaction . the maximum chlorophyll fluorescence band at 682 nm decreased and the intrinsic fluorescence emission intensity at 308 nm and 328 nm either increased or decreased
結(jié)果表明：交聯(lián)處理對psll放氧核心復(fù)合物葉綠素?zé)晒夂蛢?nèi)源熒光都有影響，引起682urn處葉綠素?zé)晒鈴姸鹊慕档汀?08urn或328urn處蛋白質(zhì)內(nèi)源熒光強度的增大或減小，并與處理時所用交聯(lián)劑的濃度、交聯(lián)劑的親疏水性和交聯(lián)臂長相關(guān)。 - the division of regional structural systems in the study area, the timing and distribution range of the ductile shearing zone and the metamorphic core complex, and their compounding were made by the author in the light of results of the synthetic study on geology in deep, geophysical prospecting, and interpretation of remote sensing image
結(jié)合深部地質(zhì)、物探和遙感解譯資料，劃分了遼東巫閭山地區(qū)構(gòu)造體系和構(gòu)造帶歸屬、韌性剪切帶與變質(zhì)核雜巖的時代、范圍分區(qū)及其復(fù)合關(guān)系。 - dongzigou ag deposit and jianbaoshan au deposit are hosted in the sandstone of middle-proterozoic suberathem, which are developed from the proterozoic sediment metal source-rocks formed during the meso-proterozoic volcanism and reworked by the mesozoic tectono-magmatism during the formation of the metamorphic core complexes in eastern hebei . the dongzigou ag deposit has the characteristics of reformed strata-bound origin, the jianbaoshan au deposit, located in the detachment fault, is the alterated rock type . both deposits have the similar wall-rock alteration, and show the same trace element behavior, and ree patterns . they are the results of the multi-stage tectono-magmatism in the environment of continental extension in eastern hebei region . their mineralization depended on their wall rocks and relative location in metamorphic core complexs
賦存于中元古宙長城系常州溝組的洞子溝銀礦床和尖寶山金礦床是由密云-都山變質(zhì)核雜巖構(gòu)造體系所控制的一組礦床。其成因為中元古宙火山巖漿活動形成的沉積礦源，后經(jīng)中生代的變質(zhì)核雜巖構(gòu)造巖漿體系疊加改造而成。洞子溝銀礦床具有層控迭加改造的特點尖寶山金礦床則具有破碎蝕變巖型礦床的特點。 - dongzigou ag deposit and jianbaoshan au deposit are hosted in the sandstone of middle-proterozoic suberathem, which are developed from the proterozoic sediment metal source-rocks formed during the meso-proterozoic volcanism and reworked by the mesozoic tectono-magmatism during the formation of the metamorphic core complexes in eastern hebei . the dongzigou ag deposit has the characteristics of reformed strata-bound origin, the jianbaoshan au deposit, located in the detachment fault, is the alterated rock type . both deposits have the similar wall-rock alteration, and show the same trace element behavior, and ree patterns . they are the results of the multi-stage tectono-magmatism in the environment of continental extension in eastern hebei region . their mineralization depended on their wall rocks and relative location in metamorphic core complexs
賦存于中元古宙長城系常州溝組的洞子溝銀礦床和尖寶山金礦床是由密云-都山變質(zhì)核雜巖構(gòu)造體系所控制的一組礦床。其成因為中元古宙火山巖漿活動形成的沉積礦源，后經(jīng)中生代的變質(zhì)核雜巖構(gòu)造巖漿體系疊加改造而成。洞子溝銀礦床具有層控迭加改造的特點尖寶山金礦床則具有破碎蝕變巖型礦床的特點。
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