鲁瓦扬

We consider the Xijinwulan- Jinshajiang suture as an additional Indosinian suture which developed within the Yangtze plate. The Bangong Co-Nujiang and Yarlung Zangbo sutures developed within the Gondwanaland domain, but neither can be con- sidered to define the northern boundary of Gondwanaland.

西金鸟兰-金沙江缝合带是发育在扬子板块内部的印支期缝合带，班公湖～怒江和印度河一雅鲁藏布江缝合带是发育在冈瓦纳大陆框架下新特提斯阶段的缝合带，构不成冈瓦纳北界。

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；不存在从古生代延续到三叠纪的大洋盆地，即不存在所谓古特提斯或永久特提斯；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支，燕山，喜马拉雅3个阶段脉动式板块汇聚造山过程。

The following provinces are part of this development: ZAMBEZI PROVINCE: Districts MORRUMBULA, PEBANE MANICA PROVINCE Districts MACHAZE, GURO, TAMBARA NAMPULA PROVINCE: Districts MOSSURIL, MEMBA, NACROA, ERATI, NACALA-A-VEHLA, LALAUA INHAMBANE PROVINCE: Districts MABOTE, FUNHALOURO, PANDA, VILANCULOS, GOVURO (in-land on rivers and on the coast) GAZA PROVINCE: Districts CHICUALACUALA, MASSANGENA, CHIGUBO, MABALANE (in-land on rivers and on the coast) TETE PROVINCE: Districts CAHORRA BASSA, CHANGARA, MACOE, MACANGA, ZUMBO, MARAVIA (north and south of the Cahorra Bassa dam) NIASSA PROVINCE: Districts NIPEPE, METARICA, CUAMBA, MANDIMBA, NGAUMA, LAGO, LICHINGA (in- land and on Lake Malawi and standing rivers) Bio-diesel will be manufactured from the oil pressed form the seed of the Jatropha curcas tree.

这项费用包括了所有的费用和必要的程序，获取土地为期50年的特许权，注册公司等，省以下是这部分的发展：全省赞： morrumbula区，佩巴内，马尼卡省地区马沙泽九老区，坦巴拉，楠普拉省：莫苏里尔地区，门巴， nacroa ，埃拉蒂，纳卡拉-- vehla ，拉拉瓦，伊尼扬巴内省：地区生病，富尼亚洛鲁，熊猫，维兰， govuro (-对土地，河流和海岸)加扎省：希夸拉夸拉区，马桑热纳，希古博，防护栏德拉卡马省：区cahorra巴萨，尚加拉， macoe ，寻购，博， maravia (南北该cahorra拉巴萨大坝)尼亚萨省：尼佩佩区，梅塔里卡，库安巴，曼丁巴， ngauma ，拉戈， lichinga (在土地和马拉维湖身高河流)生物柴油的制造将来自石油按下表种子的桐子树。

By the time of its fall, most of the prisoners were writers who had written against the corruptions of the government.

到它被攻陷的时候，里面多数的犯人是写了反对政府贪污文章的作家。

The most obvious variation to ovum morphological character was that the color was changed from light green to sepiaceous in embryonic development, and all the ovums were almost hatched after 96h.

在胚胎发育过程中卵的形态特征最明显的变化是颜色从淡绿到深褐色，卵在发育96h后卵基本全部孵化。