AN ATTEMPT AT VISUAL INTERPRETATION FOR METRIC CAMERA OF STS-9/SPACELAB
- Issue 4, Pages: 282-291(1988)
Published:1988
DOI: 10.11834/jrs.1988038
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Published:1988
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本文是利用“空间实验室定标测量相机”(Metric Camera缩写为MC)拍摄的中国西藏日喀则地区的像片
进行室内目视判读的一次尝试。文中概略介绍了1983年11月28日—12月8日
美国航天飞机第9次飞行(STS9)装载的欧洲空间实验室的MC的基本工作参数;利用其像片编制的地质判读辅助图件(水系判读图、线性影像环形影像判读图)和典型岩性、构造的判读工作
并与陆地卫星MSS图像作了简单的比较。认为MC像片的地物影像清晰
反映基岩裸露区的地质信息丰富。在MC像片上易于区别大岩类(如花岗岩类、基性一超基性岩类、正常沉积岩及火山岩等)
甚至可以发现某些地层标志层或走向上的差异;多数岩层产状可以辨认
褶皱可以定性判读;断裂判读效果很好
其规模、方向、组合都有不同程度的反映
同时
还可以判读出一些隐伏断裂。MC像片的判读效果优于MSS图像
可以满足中、小比例尺编图的要求
对中比例尺野外地质调查能起到很好的作用。
This article deals with an attempt at indoor visual interpretation of the metric camera images of Rikaze area
Tibet plateau. It briefly introduces the basic parameters of the metric camera in European spacelab carried by the spacecraft during its ninth flight (STS-9/Spacelab) from Nov. 28th
1983. The supplementary maps were mapped using MC images of geological visual interpretation (such as drainage system
lineament and circular features). The inter-pretated results of typical lithological chracters and structure were compared with Lansat MSS data. The conclusions are: (1) with MC images
the objects on ground are clear
(2) the bare area of bedrocks supplies abundant geological information
(3) the different rock unit can be easily distiguished (such as granite
basicultrabasic rocks
normal sedimentary rocks and volcanic rocks etc.)
and (4) some stratigraphic key horizons
the differentiation of strikes can be recognized
(5) most information of occurance can be identified and the fold structure can be inter-pretated qualitatively. The results of the inperpretation are very good
the dimensions
directions
combinations of the fault are reflected
and some blind faults can also be interpreted. The effects of interpretation of MC imagas excells that of the MSS images and can meet the needs of mapping standards at middle scale.
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