| 000 | 00924nam a2200229 4500 | ||
|---|---|---|---|
| 001 | 0000002710 | ||
| 008 | 111028 1992 eng d | ||
| 040 | _aJMGHQ | ||
| 090 | 0 | 0 |
_a553.6220959522 _bAZE |
| 100 | 0 | _aAzemi Eki | |
| 245 | 1 | 0 |
_aSummary if silica sand deposits in Sarawak _cAzemi Eki, George Peter Meran. |
| 260 | _c1992 | ||
| 300 |
_aviii, 71 p. _bill., maps _c30 cm |
||
| 520 | _aSilica (Si 02) is one of the commorest material in the earth's crust. Mineralogically it occurs maily as quartz, which in its promary form is found as diseeminted grains in both igneous and metamorphic rocks such as granite or quartzite, and in sedimentary rocks such as sendtone. | ||
| 650 | 0 |
_aHydrology _zSarawak |
|
| 650 | 0 |
_aGeology _zSarawak |
|
| 650 | 0 |
_aTopography _zSarawak |
|
| 650 | 0 |
_aSand _zSarawak |
|
| 650 | 0 |
_aSediments (Geology) _zSarawak |
|
| 651 | 0 | _aBintulu (Sarawak) | |
| 700 | 1 | _aMeran, George Peter | |
| 999 |
_c22074 _d22074 |
||