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OALib Journal期刊
ISSN: 2333-9721
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南海北部边缘盆地不同类型非生物成因co2成因成藏机制及控制因素
Keywords: 南海北部边缘盆地/壳源型co2,火山幔源型co2,co2运聚成藏机制,主要控制因素
Abstract:
？南海北部边缘盆地非生物成因co2资源丰富，依据通常的成因判识与划分参数(δ13cco2和3he/4he)，结合运聚成藏的具体地质条件及控制因素，可将co2成因成藏机制明确划分为泥底辟热流体控制的壳源型及壳幔混合型co2成因成藏机制和火山幔源活动及深大断裂输导控制的火山幔源型co2成因成藏机制2种类型。前者，即壳源型及壳幔混合型成因co2资源丰富储量规模大，这种成因成藏机制形成的co2运聚成藏规律复杂，主要富集于西北部走滑伸展型边缘的莺歌海盆地中央泥底辟构造带浅层，具有平面上分区、分块、纵向上分层、分带多期运聚成藏的特点，且主要受控于泥底辟热流体上侵活动与巨厚海相含钙砂泥岩的物理化学综合作用；后者即火山幔源型成因co2在该区资源及储量规模较小，多分布在处于北部裂陷带的琼东南盆地东部ⅱ断裂带周缘和珠江口盆地北部深大断裂发育区，且主要受控于火山幔源岩浆脱排气之co2气源供给与深大断裂导气输送作用的有效配置。
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