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Microgranite. In some pisces this coincides wtth a shallov slope down onto the largely unexposed basement complex, In a few places, a fault can be substantiated by the occurrence of microbrecciated microgranite, with quartz-filled fractures, or by nearby man-made exposures of the basement complex. In some sectors the faults are visible on aerial photographs but generally only weakly so. In places, the Barolong Farms Fault appears on the aerial photographs to consist of two aubparallel strands.
However, even after field and photogeological mappin8 of the faults, some uncertainty remained about their position in some sectors. Therefore a series of magnetometer traverses was made across the boundaries of the Granite and the geophysical interpretation was used to refine the geological mapping. The Granite was found to be magnetically 'noisy', with numerous anomalies of small wavelength and amplitude. The basement complex (mostly weathered granitic gneisses) was characteristically 'quiet', generating a smooth magnetometric profile. Control traverses were made where the position of the fault was accurately known, as well as the traverses in the less well-known sectors. On most profiles the position of the boundary fault was marked by an abrupt change from 'noisy' to 'quiet', in several cases with a coincident negative anomaly. In every case, this was consistent with the field and photogeological evidence although there was some ambiguity in the interpretation of one profile across the southern boundary. This ambiguity was partly resolved by postulating an unexposed fault block of Ntlhantlhe Microgranite within the boundary zone. The magnetometer traverses are described and discussed in detail by Aldiss and Bantshang
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Microgranite 。在一些双鱼座这正好wtth 1 shallov斜坡下降到地下室主要暴露复杂,在一些地方,出现故障可以证实发生microbrecciated microgranite ,石英填充骨折,或由附近的人为风险的地下室复杂。在一些部门的故障是看得见的航拍照片,但一般只弱如此。在地方,拿巴罗龙农场故障出现在空中拍摄的照片组成的两个aubparallel链。
然而,即使在外地和photogeological mappin8故障,一些不确定性仍然是他们的立场在某些部门。因此,一系列的磁强计穿越了跨越国界的花岗岩和地球物理解释是用来完善地质填图。花岗岩被认为是磁'噪音' ,有许多异常的小波长和振幅。地下室复杂(主要是风化花岗质片麻岩)是典型的'安静' ,产生一种平稳磁力形象。遍历控制了那里的立场是准确已知故障,以及遍历在较知名的部门。在大多数配置文件的位置边界断层的特点是突然改变'噪音' ,以'安静' ,在一些情况下,以同步负异常。在任何情况下,这是符合外地和photogeological证据,尽管有一些模棱两可的解释,一个剖面的南部边界。这种模棱两可的部分解决,通过假定一个暴露断块Ntlhantlhe Microgranite区范围内。遍历的磁强计和描述中详细讨论了奥尔迪斯和Bantshang
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第1个回答  2009-05-29
Microgranite。在一些双鱼座wtth此时恰逢一个shallov斜坡上,在很大程度上馀地下室复杂一些地方,可根据发生的骨折,quartz-filled microbrecciated microgranite,或者附近的人造暴露的地下室复杂。在某些领域上的缺点是可见的,但一般来说,只有航拍照片弱。在有些地方,这个Barolong农场故障出现在空中拍摄的照片是由两个aubparallel股。
然而,即使在能量场和photogeological mappin8的缺点,仍有一些不确定性在某些领域。因此一系列仪是穿过边界横贯东西的花岗岩和解释是用来提炼地质测绘。被发现的花岗岩磁性的吵闹的,与众多的小型波长和振幅。地下室的复杂(主要是饱经风霜的特点gneisses碾盘),产生了一个平滑的安静magnetometric轮廓。在控制了横贯的位置准确故障,以及横跨在少有的行业。在大多数侧面边界断裂的位置是一个突然的变化从“吵闹的“安静”,在几例与消极的异常。在每种情况下,这是符合现场和photogeological证据虽然有一些含糊不清的一个侧面诠释整个南部的边界。这个模棱两可的部分解决的假定Ntlhantlhe Microgranite馀断块内边界地带。介绍了磁力仪、横贯Aldiss详细讨论通过,Bantshang
第2个回答  2009-05-29
这么长才5分?```
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