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Search Results: 1 - 10 of 42060 matches for " 毛河光 "
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谢氏超晶石:一种FeCr2O4高压多形新矿物
陈鸣,束今赋,
科学通报 , 2008,
Abstract: 新矿物谢氏超晶石(xieite)产自于随州陨石冲击脉体中,属于斜方晶系,空间群为Bbmm,晶胞参数a=9.462(6)?,b=9.562(9)?,c=2.916(1)?.矿物实测化学式为(Fe0.87Mg0.13-Mn0.01)1.01(Cr1.62Al0.25Ti0.08V0.02)1.97O4,简化式为FeCr2O4.X射线衍射的特征谱线[d(?),I/I0](2.675,100),(2.389,20),(2.089,10),(1.953,90),(1.566,60),(1.439,15),(1.425,15),(1.337,40).在冲击波引起的高温高压作用下,谢氏超晶石通过固态反应从铬铁矿转变形成,是FeCr2O4的高压多形矿物相.共生高压矿物有林伍德石、镁铁榴石、玲根石和涂氏磷钙石等,形成的压力和温度条件分别为18~23GPa和1800~1950℃.谢氏超晶石已获国际矿物协会新矿物、命名与分类委员会批准(IMA2007-056),该矿物以中国矿物学家谢先德教授的姓氏命名.
大陆漂移的源动力—板块自驱动模式
The Source Power for Continental Drift —Plate Self-Drive Mode
 [PDF]


Advances in Geosciences (AG) , 2013, DOI: 10.12677/AG.2013.32013
Abstract:
基于作者提出的“岛弧海沟成因模式——板块漂移尾迹产生的海沟火山喷发”原理,首先从最简单的物理力学和沉积学原理出发,从理论上给出了一个板块自驱动模式,即大陆板块在划过洋壳后,留下薄弱洋壳,引起地下岩熔的上涌并产生向前的推力,在地下岩熔热力的驱动下向前漂移。然后通过几个实际例子印证该自驱动模式的普适性。最后给出了一个类比试验,说明大陆板块在大洋板块上是通过岩熔产生的热力不平衡所驱动的,就好比大陆板块自带了一个螺旋桨。
Based on the simple principle of “arc trench genetic model—the trench volcanic eruption by plates drift boundary” developed by the author, beginning from the simple physical mechanics and sedimentology principle, I give a theoretical plate self-drive mode. That is when continental plate slip across the ocean crust. It will leave a weak oceanic crust, and the underground lava upwelling will produce a force or power and generates forward thrust. So continental plates were driven by underground lava heat and caused forward drifting. Then several real examples confirm the self-drive mode is common on the Globe. At last an analog test was given which showed that continental plate in the ocean is driven by thermal, it looks like that the continental plate brought a propeller for itself.
美国黄石公园间歇泉成因机制探讨
Study on the Genesis of Geysers in American Yellowstone National Park
 [PDF]


Advances in Geosciences (AG) , 2013, DOI: 10.12677/AG.2013.33025
Abstract:
美国黄石公园内的间歇泉是一个奇特的地质景观,它们是如何形成的?目前关于黄石公园的间歇泉成因是用海底扩张和板块构造的模式解释的,但这种模式在其他地区存在自相矛盾的地方。本文结合作者提出的大陆漂移的源动力——板块自驱动模式,给出了另外一个全新的成因模式,该模式说明当大陆板块漂移时,会在板块运动的前方产生刮蹭堆积及挤压形成山脉高原,同时也可能刮起一些深海含水物质形成深部含水圈闭,该含水圈闭还会与深部岩浆连通,在板块运动中,不断接受应力变化,产生间歇泉。同时也会在板块后方形成深海沉积。通过对美国西部落基山脉的对比发现,该模型与实际情况吻合很好。该成因模型为我们重新认识北美洲地理环境成因提供了一个新的思路。
Yellowstone geyser is a unique geological landscape, how it was formed? Current explanation about Yellowstone geysers is that it was formed by seafloor spreading and plate tectonics model, but these models cannot explain in many cases and even have contradictory. Combined with the model “source power for continental drifting-plate self- driven mode” by the author, a new genetic model was given in this paper, that is when the continental plates drift, mountains and plateaus were formed in front of the plate motion by Scratching accumulation and extrusion force. It may also whip up some deep-sea water-containing material to the formation of the deep aquifer traps, and the aqueous traps also communicate with the deep magma, it will receive continuous stress changes in the movement of tectonic plates, thus produces geysers. At the same time, deep-sea sediment was formed in its rear. This model fits very well with the Rocky Mountains of North America. The genetic model provides us a new way to rethink the origin model of the North America geographical environment.
台湾岛和黄岩岛的来源研究
Study on the Origin of Taiwan and Huangyan Island
 [PDF]


Geographical Science Research (GSER) , 2013, DOI: 10.12677/GSER.2013.22006
Abstract:
基于特提斯构造演化和东南亚地块的逃逸构造理论,首先论证了东南亚众多地块被从中国青藏高原东南角挤出的必然性。然后从地理形状、山脉走向对台湾岛从菲律宾分离前的状态进行了复原,发现其吻合非常好。同时从地质、地球物理、考古和雅美人的特征分别找到了台湾岛分离的确凿证据。最后证明包括菲律宾、马来西亚、印尼等众多东南亚国家都是随着印度板块的向北挤压从中国青藏高原的东南角被挤出去,并漂移到当前位置。他们大多数是印度板块从特提斯洋底刮蹭下来的堆积岛。台湾岛最后是从吕宋岛分离而来,而黄岩岛是古华夏板块向北漂移过程中在南中国海的产物。
At first based on the Tethyan tectonic evolution and escape tectonics theory about Southeast Asia block, we find it is necessary for the Southeast Asian blocks to extrude from the southeast corner of the Ti-betan Plateau of China. And then we recover the original shape of Taiwan Island before its separation from Philippines. The recovered result show that the geographic shape, mountains direction all fit very well. At the same time, from the characteristics of geological, geophysical, archaeological and Yami people, we find clear separation evidence of Taiwan Island. Finally, we certify that most Southeast Asian countries including Phil-ippines, Malaysia, Indonesia and so on are all the result of the India Plate northward extrusion from China Qinghai-Tibet Plateau. They are the results of squeezed out materials. Most of them are accumulated island scraped down by the India Plate from the Tethys Ocean. Taiwan Island is from Luzon Island with its last sta-tion. Huangyan Island is the drifting product of the ancient Huaxia plate.
日本从中国分离出去的8大证据
Eight Evidences Show Japan Was Separated from China
 [PDF]


Geographical Science Research (GSER) , 2013, DOI: 10.12677/GSER.2013.22003
Abstract:
基于作者提出的“板块运动轨迹所产生的海底堆积和深海峡谷”这一深海峡谷成因模式,首先通过尾迹分析和大地构造演化历史给出了日本列岛的分离模式和运移轨迹,然后分别从地貌形态、山脊走向分布、地质地层、地球物理和岩石学、古生物及古气候、考古、中日文化融合及日本人和中国人的基因对比等给出8个方面的证据,证明日本分4部分分别从不同的地方分离、漂移到当前位置。主体部分3个主岛(本州、四国、九州)是从中国浙江舟山市以南至福建广东沿海分3片分别漂移到目前的位置的,其第4个主岛(北海道岛)是从太平洋中的关岛附近漂移过去的。本文的结论否认了目前日本权威地质学家所得出的“日本是从朝鲜半岛分离出来的”这个“定论”。日本列岛未分离前其东京市大约位于目前的台北市附近。钓鱼岛等岛屿是日本分离漂移过程中产生的岛屿。
Based on the arc trench genetic model developed by the author, at first through wake analysis and tectonic evolution history of the Japanese islands, I give a separation mode and the migration path for Japan, then give 8 aspects of evidence respectively from the landscape form, ridge distribution, geological formation, geophysical and paleontology and ancient climate, archaeology, the Sino-Japanese cultural fusion and Japa-nese and Chinese gene contrast. All these show that the Japan mainland was separated by 4 parts and drifted to the current position from different places. The three main islands (Honshu, Shikoku, and Kyushu) of main part were from China (from the south of Zhoushan City of Zhejiang Province to the coast of Fujian and Guangdong Provinces) by 3 pieces respectively. The fourth main island (Hokkaido Island) was from the posi-tion of Pacific Ocean near the Guam in the past. This paper has denied the final conclusion “Japan was de-rived and separated from the Korean Peninsula” by Japanese authoritative geologists. Tokyo City located ap-proximately near the current Taipei before the Japanese Islands separation. The Diaoyu Islands are the by-products in the drifting and separation of the Japanese Islands.
加拿大北部“破碎山河”的成因与大陆漂移
Study on the Relationship between the Origin of Broken Plates in Northern Canada and Continental Drift
 [PDF]


Geographical Science Research (GSER) , 2013, DOI: 10.12677/GSER.2013.22004
Abstract:
加拿大北部的“破碎山河”是地球上独一无二的,它们是如何形成的?目前关于其成因的模式一直是沿用传统的海底扩张和板块构造的模式解释的,但这种模式在其他地区存在自相矛盾的地方。本文结合作者提出的大陆漂移的源动力——板块自驱动模式,给出了一个北美洲受力模型,说明了加拿大北部破碎山河的成因。该成因模型为我们重新认识北美洲地理环境成因提供了一个新的思路。
Broken plates in northern Canada are unique on Earth, how they are formed? The current explana-tion about it is that it was formed by seafloor spreading and plate tectonics model, but this model cannot be explained in many cases and even has contradictory. Combined with the model “source power for continental drifting-plate self-driven mode” by the author, a new genetic model was given in this paper, that is the North America-force model which explains the causes of broken plates in northern Canada. The genetic model pro-vides us a new way to rethink the origin model of the North America geographical environment.
中国西藏罗布莎蛇绿岩金刚石包裹体的研究
束今赋,杨经绥,戎合,
地质学报 , 2013,
Abstract:
THE PRESSURE CALIBRATION UP TO MBARS AND THE ACHIEVEMENT OF 5.5 MBARS UNDER HYDROSTATIC AND NONHYDROSTATIC CONDITION
百万大气压下的压强校准及5.5 Mbar静压强的获得

XU JI-AN,MAO HE-GUANG,PETER BELL,
徐济安
,,PETER BELL

物理学报 , 1987,
Abstract: Pressure calibrated up to 0.8 Mbar under hydrostatic condition and to 2 Mbars under non-hydrostatic condition. We find the red shift of ruby R fluorescence to 830nm at the highest pressure point in our diamond high pressure cell. The shift correspond to 5.5 Mbars by calibration.
利用固体潮压电效应和自然电位测量勘查隐伏矿床的新方法

黄金科学技术 , 2010,
Abstract: 介绍一个原始创新的地球物理勘探新方法(国家发明专利)。该方法利用压电效应的原理,将固体潮所产生的压电效应和自然电位测量结合起来,是直接勘探石英脉型金矿和其他矿床(有压电效应)的全新方法。其实施步骤如下a)在勘查区域按网格布设不极化电极,埋植深度及要求与自然电位法勘查类似。b)对这些布设的电极进行二次电位测量一次是在固体潮高潮时测量,另一次是在固体潮低潮时测量。根据固体潮产生的压电效应,在有石英脉型金矿(或方铅矿、铅锌矿、黄铁矿、铜镍硫化物矿及多种伟晶岩等)的地段将出现二次测量的明显差异,即高固体潮时和低固体潮时测量的电位差将有明显的异常。如果在该地段处没有预期的这些类型的矿床,高固体潮时和低固体潮时测量的电位差将不会有明显的异常。
北极冰川融化的根源与地球碳丢失

地质学报 , 2013,
Abstract:
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