中国煤炭地质
中國煤炭地質
중국매탄지질
COAL GEOLOGY OF CHINA
2014年
9期
27-30
,共4页
呼鲁斯太矿区%瓦斯分布%煤变质%构造
呼魯斯太礦區%瓦斯分佈%煤變質%構造
호로사태광구%와사분포%매변질%구조
Holstay mine area%gas distribution%coal metamorphism%structure
根据煤矿井下煤层瓦斯参数测定结果,以瓦斯地质理论为基础,分析了呼鲁斯太矿区瓦斯分布规律及其控制因素。结果表明:矿区煤层瓦斯区域分布具有不均衡性,以F2-2和F22断层为界将矿区划分为北部、中部、南部三个区域,中部煤层瓦斯压力、瓦斯含量最高,北部次之,南部最低;煤变质程度较高和围岩封闭性较好是矿区瓦斯富集的根本条件,而构造复杂程度的不同、构造线方向的改变是瓦斯分布不均的主控因素。矿区中部为北北东向构造向东西向构造转折区,应力集中,且顶板为泥岩,煤变质程度较高,形成较好的瓦斯生储条件;南部北北东向推覆构造较为强烈,使煤层沿倾向切割,断层连通地表,造成瓦斯大量逸散。
根據煤礦井下煤層瓦斯參數測定結果,以瓦斯地質理論為基礎,分析瞭呼魯斯太礦區瓦斯分佈規律及其控製因素。結果錶明:礦區煤層瓦斯區域分佈具有不均衡性,以F2-2和F22斷層為界將礦區劃分為北部、中部、南部三箇區域,中部煤層瓦斯壓力、瓦斯含量最高,北部次之,南部最低;煤變質程度較高和圍巖封閉性較好是礦區瓦斯富集的根本條件,而構造複雜程度的不同、構造線方嚮的改變是瓦斯分佈不均的主控因素。礦區中部為北北東嚮構造嚮東西嚮構造轉摺區,應力集中,且頂闆為泥巖,煤變質程度較高,形成較好的瓦斯生儲條件;南部北北東嚮推覆構造較為彊烈,使煤層沿傾嚮切割,斷層連通地錶,造成瓦斯大量逸散。
근거매광정하매층와사삼수측정결과,이와사지질이론위기출,분석료호로사태광구와사분포규률급기공제인소。결과표명:광구매층와사구역분포구유불균형성,이F2-2화F22단층위계장광구화분위북부、중부、남부삼개구역,중부매층와사압력、와사함량최고,북부차지,남부최저;매변질정도교고화위암봉폐성교호시광구와사부집적근본조건,이구조복잡정도적불동、구조선방향적개변시와사분포불균적주공인소。광구중부위북북동향구조향동서향구조전절구,응력집중,차정판위니암,매변질정도교고,형성교호적와사생저조건;남부북북동향추복구조교위강렬,사매층연경향절할,단층련통지표,조성와사대량일산。
On the bases of coalmine underground gas parameter tested results and gas geology theory, analyzed coal gas distribution pat-tern and its controlling factors in the Holstay mine area. The results have shown that the mine area gas regional distribution is dispropor-tion. Taking the faults F2-2 and F22 as boundaries, divided the mine area into north, middle and south three zones;coal seams in the mid-dle zone have highest gas pressure and gas content, north zone the second, south zone lowest. High degree of coal metamorphism and good enclosing rock sealing are essential conditions for gas enrichment;while different structural complexities and structural line trend changes are main controlling factors of gas distribution disproportion. The middle zone is the turning interval of structural trend from NNE into EW, stress concentrated, coal roof is mudstone and high degree of coal metamorphism thus formed rather good gas generation and storage conditions;south zone has stronger NNE nappe structures made the coal seams dissected along the dip, then again, faults outcropped and brought about large amount gas dissipated.