Fine structures of crust and mantle and potential hot dry rock beneath the Zhangzhou Basin
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摘要:
漳州盆地与相邻地带的地质构造复杂，水热活动强烈，且伴随着小地震的频频发生.为厘定该盆地深部是否存在潜在的干热岩体，则必须对其壳、幔精细结构和介质物理属性进行探查、研究与探讨.基于漳州盆地壳幔速度结构的格局发现：（1）"灵霄-漳州-安溪"地带的深处存在一低速层，且在漳浦-长泰之间呈现出一"扁豆状"低速体；（2）该低速体北侧为一伸抵上地幔顶部、且向北倾的深大断裂带，若该"扁豆状"低速体为潜在的干热岩，则该深大断裂带可能为深部热液物质上涌与热源补给的通道.
Abstract:The Zhangzhou basin and adjacent areas are complex in geological structure with strong hydrothermal activity and frequent small earthquakes. To clarify whether hot dry rock exists beneath this region, we must explore fine structures of the crust and mantle and the properties of their media. The pattern of velocity structures in the Zhangzhou basin suggests that (1) a low velocity zone exists in the crust of the Lingxiao-Zhangzhou-Anxi area, while a lens-shaped low velocity body is present between Zhangpu and Changtai. (2) North of this low-velocity body is a deep and large fault zone that dips to north, extending to the top of upper mantle. If this lens-shaped low velocity body is potential underground hot dry rock, then this fault zone is probably a channel of upwelling hydrothermal materials and thermal source supply from deep curst and mantle.
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图 1
福建境内中新生代主要断裂构造分布图(张洁等，2016)
Figure 1.
Major Mesozoic-Cenozic faults in Fujian(Zhang et al., 2016)
图 2
福建境内主干断裂构造与温泉分布格架图(中国科学院地球物理研究所和福建省地质矿产局，1992)
Figure 2.
The distribution figure of the trunk fracture structure and thermal spring in Fujian (Institute of Geology and Geophysics, Chinese Academy of Sciences and Fujian Provincial Bureau of Geology and Mineral Resources, 1992)
图 3
福建东部陆缘地震活动特征分布示意图(黄卿团和郑韶鹏，2006)
Figure 3.
A brief distribution of distant seismic activity characteristics in East Fujian (Huang and Zheng, 2006)
图 4
不同构造单元的平均速度(km·s-1)-平均厚度分布(邓阳凡等，2011)
Figure 4.
Average velocity (km·s-1)-thickness in different units (Deng et al., 2011)
图 5
华南大陆西北向和东北向剖面的速度结构(邓阳凡等，2011)
Figure 5.
The velocity structure in northwest and northeast profiles of South China continent (Deng et al., 2011)
图 6
爆炸地震炮点与台站分布图
Figure 6.
The distribution of the shot points and the stations for explosion seismological investigation
图 7
穿越漳州盆地两条主干剖面(AA′(NNE)和BB′(近EW))中L1和L3段的P波地震记录图
Figure 7.
P and S waves seismic recording for tow trunk profiles in Southeast of Fujian province
图 8
福建东山—漳州—安溪地震壳、幔速度结构(熊绍柏等，1991)
Figure 8.
Records of the Dongshan-Zhangzhou-Anxi curst and mantle velocity structure
图 9
福建境内两条主干剖面的上永安—古雷段S波地震记录图
Figure 9.
S waves seismic recording for tow trunk profiles from Yongan to Gulei in Southeast of Fujian province
图 11
中高温或高温天然蒸气田形成与组构的示意性模型(Kappelmeyer and Haenel, 1974)
Figure 11.
A model of formation and structure of medium-high temperature or high temperature natural steam field
图 12
太平洋板块俯冲消减带上部岩浆岩与深部热储体成因模式示意图(Zhou and Li, 2000)
Figure 12.
Schematic diagram of the genetic model of upper magmatic rocks and deep thermal reservoirs in the subduction zone of the Pacific plate
表 1
各测线基本数据一览表
Table 1.
The summary of the explosion seismological profiles
测线代号 起止地点 测线长度(km) 测线走向 平均点距(km) 记录的炮点编号 记录剖面代号 备注 L1(YCA) 云霄南至安溪湖头 176 NE24° 1.1~4.0 Ⅰ1, Ⅰ2, Ⅰ3 YA
AY
CY相遇与追逐测线 L5 宁化至古田县 203 NE80° 4.0 Ⅱ1, Ⅱ2, Ⅱ3 NG 单支纵测线 L4 永安至上杭 165 SW135° 5.0 Ⅱ1, Ⅱ2, Ⅱ3
Ⅱ4, Ⅱ5, Ⅱ6YS 对Ⅱ4为单支纵测线，其余为非纵测线 L3 古雷至永安 261 NW352° 4.4 Ⅱ4, Ⅱ5, Ⅱ6 YG
GY古雷炮点30 km距离以内无记录 L2 永春至宁德 195 NE36° 4.0 Ⅱ7, Ⅱ8, Ⅱ9 YN
NY相遇测线，NY剖面用L4测线资料延长到安溪以南 
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