摘要
燕山期深成岩浆热变质作用,使二1煤层由低煤级的烟煤阶段上升到D段无烟煤三号高变质阶段,同时叠加的浅成岩浆热变质作用,使二2煤层变质程度达到E段无烟煤一号或E段无烟煤二号变质阶段,形成煤田中部煤变质程度低于东西两端的变化格局。
Hypogene magma thermal metamorphis m of Yanshan stage,makeⅡ2coal -bed from bituminous coal of lo wer coal rank rised to D section of No.3anthracite in high metamorphic stage,in the mea nwhile,the stacking epizonal magma thermal meta-morphism,make metamorphic degree o fⅡ2coal -bed reached to E section of No.1anthracite or E section of No.2anth racite.Thus formed the change pattern of coal metamorphic degree:lower degree i n the mid -part of coal -field,but hig her degree in the east and west ends of coal -field.
出处
《中国煤田地质》
2001年第3期12-14,共3页
Coal Geology of China
基金
河南省煤炭资源预测与评价研究报告部分成果1995
关键词
二1煤层
煤类
煤级
深成岩浆热变质作用
浅成岩浆热变质作用
Ⅱ1 coal -bed
coal -type
coal -rank
hypogene magma thermal metamorphism
epizonal magma thermal meta-morphism