| 000 | 01147nam a2200181 4500 | ||
|---|---|---|---|
| 001 | 0000002805 | ||
| 008 | 111108 1963 eng d | ||
| 040 | _aJMGHQ | ||
| 090 | 0 | 0 |
_a555.95115 _bHIL |
| 100 | 1 | _aHill, J. H. | |
| 245 | 1 | 0 |
_aSungei Besi Mines Ltd., Selangor _ba magnetic traverse along the eastern side of the Old Hong Fatt Mine _cJ. H. Hill. |
| 260 | _c1963 | ||
| 300 |
_a4p. _c33cm |
||
| 520 | _aLimestones overlain by Quaternary sediments are exposed along the western side of the pit while granite and granite wash are exposed on the eastern side. The contact between granite and limestone trends approximately north-south along the centre of the pit. Intrusive into granitic rocks are cassiterite-bearing veins, of variable width, striking in an easterly direction with which magnetite was thought to be associated. This mineralisation can frequently be traced along the strike by a line of ironstained float. Also striking in an easterly direction across the granite ore white quartz veins. | ||
| 650 | 0 |
_aGeology _zSelangor _zSungei Besi |
|
| 650 | 0 |
_aMineralogy _zSelangor _zSungei Besi |
|
| 651 | 0 | _aSungei Besi (Selangor) | |
| 999 |
_c22613 _d22613 |
||