Hefei basin that is located on the southern fringe of the north china plate and by the side of tan - lu fault zone is a mesozoic cenozoic continental basin 合肥盆地为一中、新生代陆相盆地,位于华北板块南缘、郯庐断裂带西侧近旁侧。
2.
Qinling fold belt is located at the junction of the north china plate and the yangtze plate , and its portion in henan province is a part of the east qinling mountains ( eqm ) 摘要秦岭褶皱带位于华北板块和扬子板块结合部位,其在河南省内的部分多划为东秦岭。
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Zhang hong , wang yongdong , shen guanglong , he zonglian , wang jun . 1999 , palaeophytogeography and palaeoclimatic implications of permian gigantopterids on the north china plate . proc . int . conf . pangea & palaeozoic transition . 167 - 168 沈光隆,张泓,王军,张双全, 2000 ,陕西渭北煤田石炭-二叠纪植物地层初步研究,第三届全国地层会议论文集。 117 - 124 。
4.
Bessie had been down into the kitchen , and she brought up with her a tart on a certain brightly painted china plate , whose bird of paradise , nestling in a wreath of convolvuli and rosebuds , had been wont to stir in me a most enthusiastic sense of admiration ; and which plate i had often petitioned to be allowed to take in my hand in order to examine it more closely , but had always hitherto been deemed unworthy of such a privilege 贝茜下楼去了一趟厨房,端上来一个小烘饼,放在一个图案鲜艳的瓷盘里,图案上画的是一只极乐鸟,偎依在一圈旋花和玫瑰花苞上。这幅画曾激起我热切的羡慕之情。我常常恳求让我端一端这只盘子,好仔细看个究竟,但总是被认为不配享受这样的特权。
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Chagan sag is a secondary tectonic unit in chagandelesu depression , northeastern yingen - eji ' naqi basin , and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate , with the character of erogenic belt . in working area and its adjacent area , the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly , intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase 查干凹陷属于银根?额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元,其盆地基底为古生代时期华北板块、哈萨克斯坦板块和塔里木板块交接部位形成的陆缘或岛弧褶皱带,具有古生代造山带的性质。研究区及邻区印支期侵入岩形成于造山带强烈挤压陆内俯冲的构造环境;燕山早期侵入岩形成于由挤压转向拉伸、造山带的增厚陆壳开始发生伸展垮塌的构造环境;早白垩世火山岩形成于造山期后进一步发生伸展垮塌的区域构造环境。
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Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin , northeastern yingen - ejinaqi basin , and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate , tarim plate and kazakstan plate 查干德勒苏凹陷属于银根?额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元。其基底为古生代时期华北板块、塔里木板块和哈萨克斯坦板块交接部位的陆缘或岛弧褶皱带,具有古生代造山带的性质。
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In this case during paleozoic , nearly east west trending arc structures resulted from the interaction between china plate and siberian plate . in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault , diaoyudao fault , okinawa fault , uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate 本文所涉及近东西向展布的弧形构造形成于古生代时期中国板块与西伯利亚板块的碰撞带,而在中生代,中国板块下的kula - pacific板块向西俯冲导致了北北东向和北东向构造(如duimadao断层、 diaoyudao断层、 okinawa断层、隆起带和沉降带)以及位于中国板块东部的火山岩浆带。