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Detailed description has been given individually to the abnormal colours, lineament and circular structure and image features on the multi-geographycal information composite image. We have studied the ore control effect of circular and lineament structure to the multimetal ore, and come to the point that the Xianghualing region is a complex ore control area by circular and lineament structure.Therefore, we build a remote sensing imag model for ore field in the region. Within the circular structure, the northwest lineament crosses the northweast lineament and forms frames that control the metal ore distribution. According to the features of the found deposits and their coherent image, we conclude that there are two symbols for ore looking.

对多源地学信息复合处理图像新发现的色异常、线性和环形构造的分布、影像特征做了较详细的叙述;并探讨了该区的环形和线性构造对多金属矿的控矿作用,认为香花岭地区是环形和线形构造的复合控矿,在此基础上建立了香花岭矿田遥感影像模式:在环形构造内,发育北西向和北东向线性构造组合,交叉成"井"字型格式,控制金属矿的分布。

The difference between the crust shortening rates in west and east direction of Tianshan, is resulted from the pushing action by Pamir and the clockwise rotation of Tarim. In the west Tianshan (west to 75°E), the convergence is caused by the push of Pamir in NNW direction, and in the east to 75°E, the difference of tectonic deformation is caused by the clockwise rotation of Tarim.

从天山南北山前断层缩短速率的东西差异分析,造成天山东西变形差异显著的原因是帕米尔北向推挤和塔里木顺时针旋转的共同作用:在天山西端(75°E以西),其挤压缩短(17mm/a)是由于帕米尔高原北北西向的推挤作用;而75°E以东的地区,其差异构造变形的原因则主要是塔里木顺时针旋转的结果。

And the results indicate that the principal stress directions in study area are mainly NE-SW, and the second substage tectonic twist made the direction deflect from North to East, but the primary direction changed little; tectonic activities during the O〓~S~D stage is some violent, most of the area are under high stresses status, and rock fracture degree is correspondingly higher, as coinciding with the drill cores observation, i.

通过数值分析,模拟了塔中Ⅰ号断裂带和塔中45井三维模拟区O〓灰岩的构造应力场和应变场,结果表明:研究区主应力方向为北东~南西向,第二期的构造扭动使其由北向东发生了一定的偏转,但总的方位变化不大;O〓~S~D时期,塔中地区构造运动较强,研究区大部分处于高应力状态,岩石破裂程度较高,而岩芯观察结果也证实了这一结果,即O〓灰岩地层中早期形成的构造结构面比较发育,单个结构面的规模也较大;C~P时期,岩石的破坏程度较早期有所提高,主要表现在两个方面,一是各局部区岩石的破坏程度普遍有所提高;二是各个级别破裂区的分布范围相应地扩大了;研究区应力分布表现出明显的不均匀性,特别是剪应力,无论是O〓~S~D时期,还是C~P时期,都有很大的差异性,特别是在小断层的端部,剪应力比较集中,而且在断层的两盘,剪应力方向和大小都变化极快。

To milk my She-goats, and manage my little Flock, in the Wood; which as it was quite on the other Part of the Island, was quite out of Danger; for certain it is, that these Savage People who sometimes haunted this Island, never came with any Thoughts of finding any Thing here; and consequently never wandred off from the Coast; and I doubt not, but they might have been several Times on Shore, after my Apprehensions of them had made me cautious as well as before; and indeed, I look'd back with some Horror upon the Thoughts of what my Condition would have been, if I had chop'd upon them, and been discover'd before that, when naked and unarm'd, except with one Gun, and that loaden often only with small Shot, I walk'd every where peeping, and peeping about the Island, to see what I could get; what a Surprise should I have been in, if when I discover'd the Print of a Man's Foot, I had instead of that, seen fifteen or twenty Savages, and found them pursuing me, and by the Swiftness of their Running, no Possibility of my escaping them.

羊群在岛的另一边,因此没有什么危险。因为那些偶尔上岛的野人,从来没有想在岛上找到什么东西,所以他们从不离开海岸向岛里走。我也毫不怀疑,自从我处处小心提防他们之后,他们还照常到岛上来过好几次。真的,我一想到我过去出游的情况,不禁不寒而栗。我以前外出只带一支枪,枪里装的也是一些小子弹。就这样我在岛上到处东走走,西瞧瞧,看看能不能弄到什么吃的东西。在这种情况下,假使碰上他们,或被他们发现,我该怎么办呢?因为,我没有多少自卫能力。或者,假定我当时看到的不是一个人的脚印,而是一二十个野人,一见到我就向我追来。他们善于奔跑,我是无论如何跑不过他们的,那我必定会落在他们手里!

Pergolas covered with deciduous vines provide self adjusting seasonal shading . A gap between the wall and planted screens should be left for ventilation and cooling .

东向和西向的开口的地方需要不同的解决方法,上午和下午阳光来自于不同的方向,这是非常难以遮挡的。

Z Pergolas covered with deciduous vines provide self adjusting seasonal shading . A 500mm gap between the wall and planted screens should be left for ventilation and cooling .

东向和西向的开口的地方需要不同的解决方法,上午和下午阳光来自于不同的方向,这是非常难以遮挡的。

In the Eogene and Neogene, Qaidam Basin experienced the multiphase tectonic movement; the paleoclimate evolved from warm-humid to arid; the water in the basin was gradually salinized; the depocenter migrated from west to east. The master factors and developmental characters of lithologic hydrocarbon reservoirs have their own particularity. Taking the fine exploration zones of the southwest hydrocarbon-rich depression in Qaidam as the key point, with the analysis of source-rock distribution, sedimentary evolution and sedimentary system distribution, the author proposes that the density difference increases after the fluvial water enters, then clam and bar sand bodies are formed easily due to density flow. Highstand system tract and transgressive system tract below the maximum flooding surface are the main exploration areas of lithologic reservoir.

柴达木盆地古近纪-新近纪经历了多期构造运动,古气候由温湿向干旱演变、湖盆逐渐咸化、沉积中心由西向东迁移的演化过程,地层岩性油气藏的主控因素和发育特征有其特殊规律,以柴达木盆地柴西南富油气凹陷精细勘探区带为重点,通过分析烃源岩展布、沉积演化和主要沉积体系展布,提出咸化湖盆在河流入湖后因密度差较大,易形成密度流等成因的各类滩坝砂体,最大湖泛面之下的高位体系域、湖侵体系域是地层岩性油气藏的主要勘探领域。

The area of Tiaozini Sandbanks locating hi the intertidal zone is very large, which has special geomorphology characters not only from East to West parallel to bank but also from South to North vertical to bank.

位于潮间带的条子泥沙洲面积广阔,不仅具有在平行于岸方向的由西向东逐渐过渡的地貌分带性特征,同时也具有在垂直于岸方向的由北向南逐渐过渡的地貌分带性特征。

So the evolution of the tidal-basin is a reduction of the whole tidal flat, which changes and evolution can provide important evidence for the whole Radiating Sandbanks.

位于潮间带的条子泥沙洲面积广阔,不仅具有在平行于岸方向的由西向东逐渐过渡的地貌分带性特征,同时也具有在垂直于岸方向的由北向南逐渐过渡的地貌分带性特征。

Geographically, the west plateau of Sichuan is belong to the east part of Qinhai-Tibet Plateau. Since the cordilleras and rivers tends toward a north-south disposition in this area, it was a large migrating channel which the minorities in the northwest China came into the west plateau of Sichuan a long time ago. When Tubo risen in Qinhai-Tibet Plateau, its force developed quickly from west to east.

地理上属于青藏高原东缘的川西高原,由于其南北向的山脉、河流走向,很早以前就是西北少数民族向南迁徙的大通道,加之以后青藏高原上吐蕃势力的兴起并由西向东迅速扩展,使这里不仅生活着藏民族大家庭中的康巴藏人、安多藏人、嘉绒藏人、白马藏人等诸多藏族分支,还有汉、回、羌……等多个民族,形成了川西高原多民族、多文化交融并存的情况。

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The split between the two groups can hardly be papered over.

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