Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料收集基础上，运用层次分析方法对辽宁省107个典型矿山地质环境现状进行评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此基础上，探讨了在基于地质观测数、钻孔数、平面图数、剖面图数断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

门山中段映秀断裂带构造岩宏观地质特征、显微构造及组构特征，论证了构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料收集上，运用层次分析方法对辽宁省107个典型矿山地质环境现状进行综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此上，探讨了在于地质观测数、钻孔数、平面图数、剖面图数断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门山中段映秀断裂带构造岩宏观地质、显微构造及组构，证了构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

现场勘察和资料收集础上，运用次分析方法对辽宁省107个典型矿山地质环境现状进行综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

此础上，探讨于地质观测数、钻孔数、平面图数、剖面图数建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门山中段映秀裂带构造岩宏观地质特征、显微构造及组构特征，论证构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料收集础上，运用层次分析方法对辽宁省107个典型矿山质环境现状进行综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此础上，探讨了在质观测、钻孔、平面图、剖面图断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门山中段映秀断裂带构造岩宏观质特征、显微构造及组构特征，论证了构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料基础上，运用层次分析方法对辽宁省107个典型矿山地质环境现状进行综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此基础上，探讨在基于地质观测数、钻孔数、平面图数、剖面图数断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门山中段映秀断裂带构造岩宏观地质特征、显微构造及组构特征，构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料收集的基础上，运用层次分法对辽宁省107个典型矿山地质环境现状进行的综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此基础上，探讨了在基于地质观测数、钻孔数、平面图数、剖面图数的断层建模法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门山中段映秀断裂带构造岩的宏观地质、微构造及组构，论证了构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在场勘察和资料收集的基础上，运用层次分析方法对辽宁省107个典型矿山地质环进行的综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此基础上，探讨了在基于地质观测数、钻孔数、平面图数、剖面图数的断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门山秀断裂带构造岩的宏观地质特征、显微构造及组构特征，论证了构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料收集的基础上，运用层次分析方法对辽宁省107个典型质环境现状进行的综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此基础上，探讨了在基于质观测数、钻孔数、平面图数、剖面图数的断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门中段映秀断造岩的宏观质特征、显微造及组特征，论证了造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料收集的，运用层次分析方法对辽宁省107个典型矿山地质环境现状进行的综合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此，探讨了在于地质观测数、钻孔数、平面图数、剖面图数的断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依龙门山中段映秀断裂带造岩的宏观地质、显微造及组，论证了造岩具有脆性和韧性两大类型，形成序次为先韧性后脆性。

Basing on the field perambulation and information collection, 107 typical mines in Liaoning Province were evaluated with Analytic Hierarchy Process.

在现场勘察和资料收集基础上，运用层次分析方法对辽宁省107个典型矿山地质环境现状进合评估。

On basis of this model, the modeling methods and modeling flow were discussed based on data source of geological observation, drillhole, ichnography and section map.

在此基础上，探讨了在基于地质观测数、钻孔数、平面图数、剖面图数断层建模方法和建模流程。

Based on the macroscopic characteristics, microstructure and fabric of the tectonite in the Yingxin fault zone,this paper proves that there are two types of tectonite, i.

依山中段映秀断裂带构造岩宏观地质特征、显微构造及组构特征，论证了构造岩具有脆性和韧性两大类型，形成序次上为先韧性后脆性。