| 松辽盆地北部徐家围子断陷下白垩统营城组火山机构类型与喷发模式研究 |
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| 引用本文： | 贺电,李江海,刘守偈.松辽盆地北部徐家围子断陷下白垩统营城组火山机构类型与喷发模式研究[J].岩石学报,2009,25(3):659-666. |
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| 作者姓名： | 贺电 李江海 刘守偈 |
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| 作者单位： | 教育部造山带与地壳演化重点实验室,北京大学地球与空间科学学院,北京,100871 |
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| 基金项目： | 国家重点基础研究发展计划（973）项目（2006CB403502） |
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| 摘 要： | 火山岩油气藏已成为我国东部中、新生代陆内裂谷盆地内一种重要的油气藏类型。松辽盆地北部徐家围子断陷营城组火山岩中形成大规模气藏，不同火山岩相对油气的储集性差异很大，因此探究断陷内火山机构类型和喷发模式成为天然气勘探开发的基础。徐家围子断陷发育中酸性火山岩，识别出层状火山、熔岩穹隆、破火山口等3种主要火山机构赋存类型。受区域垂向和斜向两期拉张作用控制，在断裂上盘、下盘和断裂带，火山机构分别以不同形式展布：断裂下盘的掀斜肩部火山机构发育、断裂带火山机构串珠状叠置、断裂上盘火山爆发强烈并形成大型徐东破火山口。徐东破火山口的形成说明岩浆侵位于地壳底部，形成扁平状的岩浆房。岩浆垂直上升喷发或沿断裂喷发，形成徐家围子断陷中心式-裂隙式火山喷发模式。
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| 关 键 词： | 徐家围子断陷 营城组 火山机构 喷发模式 破火山口 岩浆房 |
| 收稿时间： | 2008/12/12 0:00:00 |
| 修稿时间： | 1/9/2009 12:00:00 AM |
Volcanic edifice types and eruption model of Yingcheng Formation, Lower Cretaceous, in Xujiaweizi fault depression, northern Songliao Basin |
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| HE Dian,LI JiangHai and LIU ShouJie.Volcanic edifice types and eruption model of Yingcheng Formation, Lower Cretaceous, in Xujiaweizi fault depression, northern Songliao Basin[J].Acta Petrologica Sinica,2009,25(3):659-666. |
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| Authors: | HE Dian LI JiangHai and LIU ShouJie |
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| Institution: | Key Laboratory of Orogenic Belt and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belt and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belt and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China |
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| Abstract: | Volcanic hydrocarbon reservoir has already been one of the most important reservoir types in Mesozoic-Neozoic rift basin in eastern China. Volcanic rocks, mainly dacitic to rhyolitic rocks, of Yingcheng Formation in Xujiaweizi fault depression, which contain natural gas, have been the key for exploration and production, hence we must make sure volcanic edifice types and eruption model first. According to investigation, there are three types of volcanic edifices, including stratovolcano, lava dome, and caldera, in Xujiaweizi fault depression. Controlled by two phases of orthogonal and oblique extension in Xujiaweizi fault depression, there are three types of spatial patterns of volcanic edifices around the regional fault. In the footwall of fault, volcanic edifices develop; in the fault belt, there is the pattern of volcanic edifices overlapping one by one; in the hanging wall of fault, it is occupied by remarkable amount of volcanic rocks and Xudong caldera. The formation of Xudong caldera indicates that the magma chamber with low aspect ratio intruded to the bottom of crust, and then magma erupted out of the ground to form volcanic edifices. It is a center-fissure eruption model controlled by both the magma chamber and regional fault in Xujiaweizi fault depression. |
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| Keywords: | Xujiaweizi fault depression Yingcheng Formation Volcanic edifice Eruption model Caldera Magma chamber |
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