Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成盆底板，将显示壳构造等级次序和造陆性质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

断裂带控制了福建区新生代壳变形和现今壳南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为描述壳块微损伤各向异性，引裂纹密度表示损伤张量形式。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气幕式移与幕式都与壳幕式构造活相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基底断裂不发育且构造稳定区域原油沥青,其稀土模式具有与上壳沉积岩相似特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐矿物并且有相似属性,包括正长石,钠长石以及拉长石.长石构成了60%上层壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期成的盆地底板，将显示地壳造的等级次序和造陆性质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

断裂带控制了福建地代地壳变形和现今地壳运动的南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为描述地壳块体微损伤的各向异性，引裂纹密度表示的损伤张量形。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气运移与地流体的流动都与地壳的造活动相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基底断裂不发育且造稳定的域原油沥青,其稀土模具有与上地壳沉积岩相似的特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐的矿物并且有相似的属性,包括正长石,钠长石以及拉长石.长石成了60%的上层地壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

同时期生成的盆地底板，将显示地壳构造的等和造陆性质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

带控制了福建地区新生代地壳变形和现今地壳运动的南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为描述地壳块体微损伤的各向异性，引纹密度表示的损伤张量形式。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气幕式运移与地流体的幕式流动都与地壳的幕式构造活动相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基底发育且构造稳定的区域原油沥青,其稀土模式具有与上地壳沉积岩相似的特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐的矿物并且有相似的属性,包括正长石,钠长石以及拉长石.长石构成了60%的上层地壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成的盆地底板，将显示地壳构造的等级次序和造陆质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

断带控制了福建地区新生代地壳变形和现今地壳运动的南北差。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为描述地壳块体微损伤的各向，度表示的损伤张量形式。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气幕式运移与地流体的幕式流动都与地壳的幕式构造活动相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基底断不发育且构造稳定的区域原油沥青,其稀土模式具有与上地壳沉积岩相似的特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐的矿物并且有相似的属,包括正长石,钠长石以及拉长石.长石构成了60%的上层地壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成的盆地板，将显示地壳构的等级次陆性质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

裂带控制了福建地区新生代地壳变形现今地壳运动的南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为描述地壳块体微损伤的各向异性，引裂纹密度表示的损伤张量形式。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气幕式运移与地流体的幕式流动都与地壳的幕式构活动相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在裂不发育且构稳定的区域原油沥青,其稀土模式具有与上地壳沉积岩相似的特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐的矿物并且有相似的属性,包括正长石,钠长石以及拉长石.长石构成了60%的上层地壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成的盆底板，将显示壳构造的等级次序和造陆性质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

断裂带控制了福建区新生代壳变形和现今壳运动的南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为壳块体微损伤的各向异性，引裂纹密度表示的损伤张量形。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

幕运移与流体的幕流动都与壳的幕构造活动相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基底断裂不发育且构造稳定的区域原沥青,其稀土模具有与上壳沉积岩相似的特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐的矿物并且有相似的属性,包括正长石,钠长石以及拉长石.长石构成了60%的上层壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成盆地底板，将显示地壳构造等级次序和造陆性质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

断裂带控制了福建地区新生代地壳变形和现今地壳运动南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为描述地壳块体微损伤各向异性，引裂纹密度表示损伤张量形式。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气幕式运移与地流体幕式流动都与地壳幕式构造活动相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基底断裂不发育且构造稳定区域原油沥青,其稀土模式具有与上地壳沉积岩相征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐矿物并且有相属性,包括正长石,钠长石以及拉长石.长石构成了60%上层地壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成的盆地板，将显示地壳构造的等级造陆性质。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

带控制了福建地区新生代地壳变形现今地壳运动的南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

为描述地壳块体微损伤的各向异性，引纹密度表示的损伤张量形式。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气幕式运移与地流体的幕式流动都与地壳的幕式构造活动相辅相成、互为因果。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基不发育且构造稳定的区域原油沥青,其稀土模式具有与上地壳沉积岩相似的特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐的矿物并且有相似的属性,包括正长石,钠长石以及拉长石.长石构成了60%的上层地壳.

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成的盆地底板，将显示地壳构造的等级次序和造陆。

Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.

裂带控制了福建地区新生代地壳变形和现今地壳运动的南北差异。

To describe the anisotropy of microdamage of the crust block, we use the damage tensor that is expressed in the fissure density.

描述地壳块体微损伤的各向异，引裂纹密度表示的损伤张量形式。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气幕式运移与地流体的幕式流动都与地壳的幕式构造活动相辅相成、互。

The REE patterns for bitumen is similar to those for supracrustal sedimentary rocks in areas with no basement faults but stabilized structural settings.

在基底裂不发育且构造稳定的区域原油沥青,其稀土模式具有与上地壳沉积岩相似的特征。

The feldspar group contains tectosilicate minerals with similar properties, including orthoclase, albite and labradorite. Feldspars make up more than 60% of the upper crust of the earth.

长石系列包含网状矽酸盐的矿物并且有相似的属,包括正长石,钠长石以及拉长石.长石构成了60%的上层地壳.