The Qinghai-tibet plateau will be Our country's biggest mineral treasure
2011-08-09 16:58阅读：
The Tibetan Plateau (Qinghai
Tibet Plateau, or Tibetan-Plateau), China's 
largest Plateau, the world average the highest elevation of the
Plateau. Most in southwest China, including the Tibet autonomous
region and the western Sichuan, Qinghai province all, Xinjiang
uygur auton
omous region in the south, and part of the Gansu, Yunnan. The
entire Tibetan plateau also included Bhutan, Nepal, India,
Pakistan, Afghanistan, Tajikistan, Kyrgyzstan, part of the total
area of 250 square kilometers. China covers an area of 240 square
kilometers, an average altitude of 4000 ~ 5000 m, has \'the roof of
the world\' and \'third pole,\' said. It's
the birthplace of
many Asian rivers. The highest level, the southwest ladder is the
Qinghai-tibet plateau. Face an average
altitude of 4000 ~ plateau 5000 m. In the Qinghai-tibet plateau
lives The Himalayan Mountains (Himalaya, Himalayas, Himalayan
Mountains HTML)
Asian majestic mountains the
Himalayas, including the world with the highest mountains, there
are more than 110 peaks up to or more than an altitude of 7300
meters (24000 feet),). One of them is the world's highest peak of
Mount Everest (Tibetan Qomolangma, western films Everest (Mount
Everest), SaJiaMa tower peak), as high as 8844.43 meters (29017.16
feet). The mountain peak in the gigantic Britain stood above the
snowline permanent. For thousands of years, the Himalayas for south
Asian nation produced the personification of deep influence its
literature, political, economic, myth, and religious reflect this.
The glacial peak would have attracted the attention of
ancient India the pilgrims, they according to Sanskrit word hima
(snow) and alaya (domains) for this magnificent mountains created
the Himalayas the Sanskrit name. Now the Himalayas is the world
climbers the most attractive place, also offered them the biggest
challenge.
The Himalayan mountains
The mountains form of the
Indian subcontinent and its northern border with north between
mainland almost impassable barrier from north Africa, is to
southeast Asia Pacific coast around half the world's large part of
orogenic belt. The Himalayas ontology in the state of Jammu and
Kashmir (Jammu Kashmir)-the disputed area of Nanga
Parbat 【 Nanga Parbat, peak is 8126 metres (26660 feet),
the world summit 】 to Tibet 9
NaJiaBaWaFeng
【 7756
meters (25445 feet) 】 between, from west to east across the
continuous 2500 km. Two Himalayan kingdom Nepal and Bhutan
mountains located in the west and east between the two. The
Himalayan mountains in the northwest and kush and the karakoram
mountains north of the border, in Tibet plateau and borders. The
Himalayas from the south to the north, in the width of 201 to 402
kilometers (125 ~ 250 miles between). A total area of about 594400
square kilometers (229500 square miles).
The geographical
position
The Himalayan mountains
The Himalayas is the highest
in the world most majestic mountains. It stands on the Tibetan
plateau, distribution in southern China's Tibet and Pakistan,
India, Nepal and Bhutan in countries such as China, its main parts
in China and Nepal junction. West up the Pamirs plateau nanga
parbat peak, east to the Yarlung zangbo river in the NaJiaBaWaFeng
sharp turn, about 2500 miles (kilometers) wide and 200 300
kilometers.
27 °
longitude and latitude: 'N, 86 ° 59 56' E (27 degrees north
latitude, longitude 86 degrees 59 points 56
points).
Located in Asia between
China and Nepal, distribution in Qinghai-tibet plateau, the
southern west Kashmir nanga parbat peak-north latitude (35 ° 14 '21
\', longitude 74 ° 35' 24 \', elevation 8125 meters), east to the
corner NaJiaBaWaFeng the Yarlung JiangDa (29 ° latitude 37 '51 \',
95 ° east longitude' 31 \', elevation 7756 meters), 2400 kilometers
long. Peak of mount Everest altitude 8844.43 meters. The Himalayas
the most typical characteristics is soaring in the height, one side
of the mountain peaks, uneven steep amazing valleys and more than
high
The Himalayan mountains
Mountain glacier erosion,
was deeply cut terrain, river valley, the totality of the
complicated geological structure, performance plants and climate
different ecological out of contact with the series (or district)
altitude. From the south to see, the Himalayas is like a curved
crescent, main beam axis of the huge beyond, snow, high mountains
above snowline glaciers and ice water supply to the bottom all
avalanche, the latter to become most the Himalayas the sources of
the river. However, most of the Himalayas is under the snowline.
The Himalayan mountains can be divided into 4 parallel of the
different width of the longitudinal, all the orogenic belt orogenic
belt with distinctive characteristics and their terrain geologic
history. They are from the south to the north was named the
Himalayan mountains or inferior; Small or low the Himalayas; Big or
high Himalayan mountains; And tethys or Tibet the Himalayas.
The Himalayas things more
than 2400 km north and south, about 200-300 km wide, from a few
roughly parallel columns of mountains, southward component
protruding arc, in China and Nepal is the main part of the
territory of it. Average altitude of 6000 meters, is the world's
most majestic mountains. 7000 meters above the peak of the 40
seats, 8000 meters above the peak of 11 cities (as of 1997, 8000
meters above the world only 15), a peak peak of mount Everest
elevation 8844.43 meters, is the first peak.
Why to say the Qinghai-tibet
plateau will be our country's biggest mineral treasure? The
formation of this and it has a great contact.
In the Qinghai-tibet plateau
have definitive evidence that can be traced back to the geological
history of about 4 500 million years ago, followed by the Tibetan
areas of the gastropods parts had different material of the earth's
crust and lift, or for submerged, or for the land. To 280 million
years ago (geological s early Permian), now of the Qinghai-tibet
plateau is the vast ocean surges. The sea area in the south of the
continent now across Europe, and north Africa in southern Europe,
southeast Asia, west Asia and the sea, known as the \'communication
tethys sea\', or \'the ancient Mediterranean\', when the tethys sea
region climate warm, became the move, plant development prosperous
region. The northern side is already was divided open original
ancient land (also called the mainland), south says gondwana
continent, include now South America, Africa, Australia, Antarctica
and south Asian subcontinent; On the north side of the continent,
also called Eurasian continent, including the cosmopolitan now
Europe, Asia and North America. Why on earth did the area sink into
an ocean?
In the plate in sports?\'
The article, the author has discussed on the issue
Isn’t it
a big comet impacts and formation of those
mountains, deep cut concave ground, deep valleys, and the rippling
namucuo basin, and so on,they are the comet hit. At the time of the
explosion had hit the area. Hit the earth's crust that rupture
caved in, the impact of the explosion of lava pushing the mantle,
which raised high mountains on both sides. When the area for ocean,
made the Himalayas become the sea island. Of course the
comets mineral alight upon those cracks in the deep. Such as
structure, and at the bottom of the lake basin and some of the
grand canyon. (play a not appropriate analogy, if the earth one
day, the center of it, is also the core will put out completely
cooling lava, at that time, if for some reason it exploded and
completely apart. So the earth's most easy to shatter material
should be surface sediments, and then is the rock of the earth \',
the last is the core in the centre of the earth. Because it is made
from many kinds of metal alloy material, not so easily broken. The
planet as well. I guess material comet may be a short life of
a star, the core materials of the star are not
even easily broken.)
The Himalayan region complex
tectonic environment at that time, the intensity of the impact is
immeasurable heavy. Another is to show the hard hit material level.
It is no doubt as the core of the metal and mineral. Also is the
core of the planet from space material. From the
distribution of terrain analysis, these minerals, most of which are
in China. 
Since 1995, China, the
United States and Canada scientist geological structure of the
Tibet detection together, the three countries' scientists measured
electromagnetic acoustic technology on the earth crust Tibet for
structure detection. As a result, they found that the Tibetan
plateau, about 100 kilometers underground in the depth of the
conductive rate is as high as 03000 to 20000 Siemens, is typical of
the continent of stable 10 to 100 times. From 1995 to 2004, three
countries' scientists spent 10 years time, proved the high Tibetan
plateau conductive characteristics is not a specific area of the
unique phenomenon, but the entire Tibetan regions of the earth's
crust characteristics. 
Generally speaking, the
conductivity of the solid rock is very poor, but high conductor
material generally for metal, graphite, clean water or seawater or
hot spring. This fully describe the Tibetan plateau underground
contain large minerals. Because the Qinghai-tibet plateau is a
piece of the ancient sea, that these minerals may experience the
years of the sediment ramming. So they will be in very deep
formation under the thick sendimentary
rock.
So the Qinghai-tibet plateau
will be our country's biggest mining
treasure!
青藏高原将是我国最大的矿产宝库
青藏高原（Qinghai-Tibet
Plateau，或Tibetan Plateau），中国最大的高原，世界平均海拔最高的高原。大部在中国西南部，包括西藏自治区和青海省的全部、四川省西部、新疆维吾尔自治区南部，以及甘肃、云南的一部分。整个青藏高原还包括不丹、尼泊尔、印度、巴基斯坦、阿富汗、塔吉克斯坦、吉尔吉斯斯坦的部分，总面积250万平方公里。境内面积240万平方公里，平均海拔4000～5000米，有“世界屋脊”和“第三极”之称。是亚洲许多大河的发源地。， 西南部最高的一级阶梯是青藏高原。高原面平均海拔4000～5000 m。在青藏高原上雄踞着
鸟瞰青藏高原
喜马拉雅山脉（Himalaya
Range, Himalayas, Himalayan Mountains）
亚洲雄伟的山脉喜马拉雅山脉，包括世界上多座最高的山，有110多座山峰高达或超过海拔7,300米（24,000英尺)、）。其中之一是世界最高峰珠穆朗玛峰（藏语Qomolangma，西方通称埃佛勒斯峰（Mount Everest），萨加玛塔峰），高达8844.43米（29,017.16英尺）。这些山的伟岸峰颠耸立在永久雪线之上。数千年来，喜马拉雅山脉对于南亚民族产生了人格化的深刻影响，其文学、政治、经济、神话和宗教都反映了这一点。冰川覆盖的浩茫高峰早就吸引了古代印度朝圣者们的瞩目，他们据梵语词hima(雪)和alaya(域)为这一雄伟的山系创造了喜马拉雅山这一梵语名字。如今喜马拉雅山脉为全世界登山者们最具吸引力的地方，同时也向他们提出最大的挑战。
喜马拉雅山脉
该山脉形成印度次大陆的北部边界及其与北部大陆之间几乎不可逾越的屏障，系从北非至东南亚太平洋海岸环绕半个世界的巨大山带的组成部分。喜马拉雅山脉本体在查谟和克什米尔（Jammu and Kashmir）有争议地区的南迦帕尔巴特峰【Nanga Parbat，8,126米（26,660英尺），世界第九高峰】至西藏南迦巴瓦峰【7,756米（25,445英尺）】之间，从西向东连绵不断横亘2,500公里。两个喜马拉雅山王国尼泊尔和不丹位于山脉东、西两端之间。喜马拉雅山脉在西北与兴都库什山脉和喀喇昆仑山脉交界，在北面与西藏高原接壤。喜马拉雅山脉从南至北的宽度，在201～402公里（125～250英里）之间。总面积约为594,400平方公里（229,500平方英里）。
地理位置
喜马拉雅山脉
喜马拉雅山是世界上最高大最雄伟的山脉。它耸立在青藏高原南缘，分布在我国西藏和巴基斯坦、印度、尼泊尔和不丹等国境内，其主要部分在我国和尼泊尔交接处。西起帕米尔高原的南迦帕尔巴特峰，东至雅鲁藏布江急转弯处的南迦巴瓦峰，全长约2500公里，宽200-300公里。
经纬度：27° 59' N, 86° 56' E（北纬27度59分，东经86度56分）。
位于亚洲的中国与尼泊尔之间，分布于青藏高原南缘，西起克什米尔的南迦－帕尔巴特峰（北纬35°14'21'，东经74°35'24'，海拔8125米），东至雅鲁藏布江大拐弯处的南迦巴瓦峰（北纬29°37'51”，东经95°03'31”，海拔7756米），全长2400公里。主峰珠穆朗玛海拔高度8844.43米。喜马拉雅山脉最典型的特征是扶摇直上的高度，一侧陡峭参差不齐的山峰，令人惊叹不止的山谷和高
喜马拉雅山脉
山冰川，被侵蚀作用深深切割的地形，深不可测的河流峡谷，复杂的地质构造，表现出动植物和气候不同生态联系的系列海拔带(或区)。从南面看，喜马拉雅山脉就像是一弯硕大的新月，主光轴超出雪线之上，雪原、高山冰川和雪崩全都向低谷冰川供水，后者从而成为大多数喜马拉雅山脉河流的源头。不过，喜马拉雅山脉的大部却在雪线之下。喜马拉雅山脉可以分为4条平行的纵向的不同宽度的山带，每条山带都具鲜明的地形特征和自己的地质史。它们从南至北被命名为外或亚喜马拉雅山脉；小或低喜马拉雅山脉；大或高喜马拉雅山脉；以及特提斯或西藏喜马拉雅山脉。
喜马拉雅山脉东西绵延2400多公里，南北宽约200－300公里，由几列大致平行的山脉组成，呈向南凸出的弧形，在中国和尼泊尔境内是它的主干部分。平均海拔高达6000米，是世界上最雄伟的山脉。海拔7000米以上的高峰有40座，8000米以上的高峰有11座（截止1997年，全世界8000米以上高峰仅15座），主峰珠穆朗玛峰海拔 8844.43米，为世界第一高峰。
为什么说青藏高原将是我国最大的矿产宝库呢。这与它的形成有着极大的联系。
就是在青藏高原有确切证据的地质历史可以追溯到距今4-5亿年前的奥陶纪，其后青藏地区各部分曾有过不同资料的地壳升降，或为海水淹没，或为陆地。到2.8亿年前（地质年代的早二叠世），现在的青藏高原是波涛汹涌的辽阔海洋。这片海域横贯现在欧亚大陆的南部地区，与北非、南欧、西亚和东南亚的海域沟通，称为“特提斯海”、或“古地中海”，当时特提斯海地区的气候温暖，成为海洋动、植物发育繁盛的地域。其南北两侧是已被分裂开的原始古陆（也称泛大陆），南边称冈瓦纳大陆，包括现在的南美洲、非洲、澳大利亚、南极洲和南亚次大陆；北边的大陆称为欧亚大陆，也称劳亚大陆，包括现在的欧洲、亚洲和北美洲。究竟这一区域是这样凹陷为海洋的呢？
在《板块在运动吗？》一文中，笔者就已经论述过有关问题
就是一颗特大彗星撞击而形成的，那些深深切割的山间凹地，深不可测的河谷，还有碧波荡漾的纳木错等等湖盆。都是当时撞击爆炸的裂痕。撞击使得地壳破裂下陷，爆炸的冲击力推挤地幔下的熔岩，从而两边凸起高高的山脉。当这一区域沦陷为海洋的时候，喜马拉雅山便成为海面上的岛屿。当然那些彗星带来的矿物就会落到那些裂痕的深处。比如构造湖底，还有盆地底部和一些大峡谷底。（打一个不恰当的比喻，假如地球有一天，它的中心将熄灭，也就是地核熔岩完全冷却，到那时候，它如果因为某种原因爆炸了而完全分裂。那么地球上最容易被粉碎的物质应该是表面的沉积岩，然后是地球逐级岩层，到最后才是地核。因为它是多种金属的合金物质，不那么容易破碎。外星球的物质也一样。我猜想彗星可能是一颗短寿命的恒星残核，那它最核心的物质就更不容易破碎了。）
喜马拉雅山区的复杂构造环境，说明当时撞击的力度之大是无法估量的。另一个就是说明撞击物质的坚硬程度。它无疑是和地核一样的金属矿物。也就是来自外来星球的核心物质。从地形的分布来分析，这些矿物的大多数都在中国境内。
自1995年开始，我国，美国和加拿大的科学家一起探测西藏的地质结构，三国科学家采用大地电磁测声技术对西藏地壳进行了结构探测。结果他们发现，西藏高原地下100公里左右的深度内的导电率高达0.3万至2万西门子，是典型稳定大陆的10至100倍。从1995年到2004年，三国科学家花了十年时间，证明了上述高导电特征并非西藏高原某个地区的独特现象，而是整个西藏地区地壳下的特征。
通常来说，固体岩石的导电性很差，而高导体物质一般为金属、石墨、干净的水或海水或温泉等。这完全说明西藏高原的地下蕴藏着大量的矿物。因为青藏高原原是一片古海，那这些矿物可能经历了上亿年的沉积物的夯实。所以它们会在很深的地层之下。
因此青藏高原将是我国最大的矿场宝库！
