Cretaceous light flesh pink granite porphyry, early Cretaceous flesh pink syenite
porphyry, and early Cretaceous light gray fine-grained quartz monzodiorite.
③ Structure
The site in A city of a province in Southeast China includes Wuyi-Daiyun fold belt
and the middle of Taiwan Strait zone of subsidence. The project site is located in
the volcanic fault sag zone in eastern Fujian of Wuyi-Daiyun fold belt, and is close
to northwest Fujian uplift zone and southwest Fujian depression zone to the west,
and Taiwan Strait zone of subsidence to the east.
The eastern Fujian volcanic fault sag zone is located in the eastern part of a
province in Southeast China, that is, east of the Zhenghe-Haifeng fault zone. On the
basis of the Variscan-Indosinian folded downwarping zone, large-scale fault subsidence and depression occurred in the Mesozoic era, forming a huge thick
Mesozoic volcanic rock zone along the southeast coast, and forming strong regional
metamorphism and migmatization along the tectonic zone, and Mesozoic magma
intruded extensively. The overall axial direction of the structure in the region is
NNE, and there is a Nanling latitudinal tectonic zone in the region, and the NW
structure crosses the region obliquely.
According to the Seismological Records of A city in a province in Southeast
China, A city in a Province in Southeast China does not have the structural
Overburden soil works of the landfill area
Seepage control of slope in the area
Landfill operation of Phase II landfill area
Landfill leachate regulating tank
Fig. 5.32 Project display
226
5 Application Cases
porphyry, and early Cretaceous light gray fine-grained quartz monzodiorite.
③ Structure
The site in A city of a province in Southeast China includes Wuyi-Daiyun fold belt
and the middle of Taiwan Strait zone of subsidence. The project site is located in
the volcanic fault sag zone in eastern Fujian of Wuyi-Daiyun fold belt, and is close
to northwest Fujian uplift zone and southwest Fujian depression zone to the west,
and Taiwan Strait zone of subsidence to the east.
The eastern Fujian volcanic fault sag zone is located in the eastern part of a
province in Southeast China, that is, east of the Zhenghe-Haifeng fault zone. On the
basis of the Variscan-Indosinian folded downwarping zone, large-scale fault subsidence and depression occurred in the Mesozoic era, forming a huge thick
Mesozoic volcanic rock zone along the southeast coast, and forming strong regional
metamorphism and migmatization along the tectonic zone, and Mesozoic magma
intruded extensively. The overall axial direction of the structure in the region is
NNE, and there is a Nanling latitudinal tectonic zone in the region, and the NW
structure crosses the region obliquely.
According to the Seismological Records of A city in a province in Southeast
China, A city in a Province in Southeast China does not have the structural
Overburden soil works of the landfill area
Seepage control of slope in the area
Landfill operation of Phase II landfill area
Landfill leachate regulating tank
Fig. 5.32 Project display
226
5 Application Cases