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3Â¥2012-06-06 09:21:01
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Сľ³æ: ½ð±Ò+0.5, ¸ø¸öºì°ü£¬Ð»Ð»»ØÌû
ggisky: »ØÌûÖö¥ 2012-06-06 09:21:08
Сľ³æ: ½ð±Ò+0.5, ¸ø¸öºì°ü£¬Ð»Ð»»ØÌû
ggisky: »ØÌûÖö¥ 2012-06-06 09:21:08
ËÓ¢Îĺõĸø·ÒëһϠ![]() Allochem is a term introduced by Folk to describe the recognisable 'grains' in carbonate rocks. Any fragment from around ½mm upwards in size may be considered an allochem. Examples would include ooids, peloids, oncolites, pellets, fossil or pre-existing carbonate fragments. Fragments are still termed allochems if they have undergone chemical transformations - for example if an aragonite shell were to dissolve and be later replaced by calcite, the replacement would still be deemed an allochem.[2] The allochems are typically embedded in a matrix of micrite (lime mud) or sparry calcite |

2Â¥2012-06-05 21:09:22














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