北昆仑碰撞造山作用,northern Kunlun collisional orogeny
1)northern Kunlun collisional orogeny北昆仑碰撞造山作用
2)collisional orogenesis碰撞造山作用
1.The controls of thecollisional orogenesis in the Qinling Mountains on the Carboniferous-Permian transgressional processes in North China;论秦岭碰撞造山作用对华北石炭二叠纪海侵过程的控制
2.Thecollisional orogenesis in the area occurred in the Carboniferous and Permian, and shows the character of the early compression and late extension.该区的碰撞造山作用主要发生在石炭纪和二叠纪,并经历了先挤压后伸展的演化过程。
英文短句/例句
1.The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny.前陆盆地的终结标志着碰撞造山作用的结束。
2.HIMALAYAN COLLISION OROGENESIS AND FORMATION OF THE LARGE ENRICHED MINERAL DISTRICT: SCIENTIFIC PROBLEMS AND THINKING喜马拉雅碰撞造山作用与(超)大型矿集区的形成:科学问题与思考
3.METAMORPHISM EVOLUTION OF THE LATE ARCHEAN COLLISION OROGENIC BELT IN WUTAISHAN五台山晚太古代碰撞造山带的变质作用演化
4.Early Paleozoic Collisional Orogeny and Magmatism on Northern Margin of the Qaidam Basin柴达木盆地北缘早古生代碰撞造山及岩浆作用
5.The Metallogeny of the Miocene Gangdese Porphyry Copper Belt in Tibetan Collisional Orogen;西藏碰撞造山带冈底斯中新世斑岩铜矿成矿作用研究
6.TECTONIC EVOLUTION OF THE LATE ARCHEAN WUTAISHAN COLLISION OROGEN五台山晚太古代碰撞造山带构造演化
7.island arc-island arc collision岛弧对岛弧碰撞作用
8.IDENTIFICATION OF SOUTHEASTERN FUJIAN MESOZOIC COLLISIONAL OROGENIC BELT闽东南中生代碰撞造山带的确认证据
9.Porphyry Cu deposits in collisional orogen setting:A preliminary genetic model初论碰撞造山环境斑岩铜矿成矿模型
10.South Tianshan: a Late Paleozoic or a Triassic orogen?南天山:晚古生代还是三叠纪碰撞造山带?
11.The Triassic Post-collisional Magmatism for the Southern Lancangjiang Tectonic Zone, Southwestern China: Petrogenesis and Its Tectonic Implications;澜沧江南带三叠纪碰撞后岩浆作用、岩石成因及其构造意义
12.VOLCANO-MOLASSE GEOLOGICAL STRUCTURE AND GEOCHEMICAL SIGNATRE IN DEVONIAN PERIOD COLLISION OROGENIC IN BEISHAN,GANSU-INMONGOLIA北山泥盆纪碰撞造山火山－磨拉石地质构造及地球化学特征
13.Present Hydrothermal Activities during Collisional Orogenics of the Tibetan Plateau;青藏高原碰撞造山过程中的现代热水活动
14.hit lightly with a picking motion.用挑选的动作轻轻地碰撞。
15.The Early Precambrian Collisional Orogenic Process and Plate Tectonics: Chance and Challenge of Precambrian Geology早期碰撞造山过程与板块构造:前寒武纪地质研究的机遇和挑战
16.Cenozoic Geological Evolution of Tanggula Mountain in the Hinterland of Qinghai-Tibetan Plateau and It Respond in Collision Effect of India-Asia Plate;青藏高原腹地唐古拉山新生代地质事件及其对印—亚板块碰撞作用的响应
17.The temporal and spatial evolution of orogenic granitic belt shows certain kind of regularities: subduction type granites→collision type granites→extensional type granites.造山带花岗岩的时空演变规律是：俯冲型→碰撞型→伸展型。
18.The frequency dispersions of Rayleigh waves and 3-D velocity structures in Himalayan collision orogenic zone and Qiangtang basin喜马拉雅碰撞造山带和羌塘盆地的瑞雷波频散与三维速度结构
相关短句/例句
collisional orogenesis碰撞造山作用
1.The controls of thecollisional orogenesis in the Qinling Mountains on the Carboniferous-Permian transgressional processes in North China;论秦岭碰撞造山作用对华北石炭二叠纪海侵过程的控制
2.Thecollisional orogenesis in the area occurred in the Carboniferous and Permian, and shows the character of the early compression and late extension.该区的碰撞造山作用主要发生在石炭纪和二叠纪,并经历了先挤压后伸展的演化过程。
3)collision orogenesis碰撞造山作用
1.The mineralizing time of skarn gold deposits is mainly of late Mesozoic (Yanshanian),contemporaneous with thecollision orogenesis occurred in the mainland of China; the gold orebodies emplaced in the late stage of thecollision orogenesis.中国矽卡岩型金矿床的成矿时间与其所在地区最晚的碰撞造山作用时间吻合，就位于碰撞造山作用的晚期；中国矽卡岩型金矿床分布在碰撞造山带、断裂岩浆带和陆缘活动带，它们都经历了强烈的显生宙碰撞造山作用；成矿地球动力学背景为碰撞造山作用的挤压－伸展转变期。
4)collisional orogeny碰撞造山作用
5)post-orogenic collision造山后碰撞作用
6)collision-type orogeny碰撞型造山作用
延伸阅读
胞饮作用和胞吞作用胞饮作用和胞吞作用pinocy tosis and endocytosis吸收膜外吸附的溶液或物质.例如大分子或分子的聚集体(moleeular aggregates)，如图所示。一般胞饮作用是指以这种方式吸收液体徽滴的过程，胞吞作用是指吸收大分子或分子聚集体的过程，但有时也用胞饮作用或胞吞作用泛指通过质膜内陷吸收膜外所吸附的物质的过程。通常这种过程在矿质养分吸附中的作用不大，但胞饮作用或胞吞作用为大分子的吸收提供了一种可能的机理。(饶立华)胞饮作用和胞吞作用(pinocy‘0515 and“n-docytosis)细胞外的液体徽滴或物质吸附在质腆上，通过质膜内陷形成小囊泡而被消化吸收的过程。电镜观察的资料证明植物根可以通过质膜内陷的方式脆饮作用及胞吞作用示意图(a)质膜外吸附大分子及液滴，(b)质膜在吸附大分子及液滴的部位内陷.(c)质膜内陷部位形成的小t泡进入细胞质，(d)小续泡膜溶解。其内含物转移到细胞质中
