GE_3DMod_PoBasin – View Service

The geological 3D model of the Po Basin includes the geometry of four stratigraphic horizons (top or Unconformity) bounding lithological homogeneous successions of sedimentary units, in the Triassic – Pleistocene time interval, and 179 fault geometries. Each stratigraphic horizon is supplemented by its isobaths. Where possible, the thickness of the succession above or below, again for basal Unconformity and top, is provided with the depth of the surface. The lithology, event process and age of each sedimentary succession are also provided. Each fault, with its upper tip line, is supplemented with the kinematic, mean values for strike, dip azimuth and dip derived from the 3D surface geometry, and the age of the oldest and younger faulted or deformed stratigraphic horizon, if Obtainable from the 3D geological model. This dataset and the related data model were obtained in the framework of the GO-PEG (https://www.go-peg.eu/) project, co-funded by the Connecting Europe Facility (CEF) of the European Commission. More specifically, this dataset is the output of the go-depth use case aiming to provide a methodology and a model to conceptualise, organise and deliver easy-to-use, high-quality, interoperable subsurface information for sustainable planning and use of natural resources. To this aim the data coming from European funded projects GeoMol (Alpine Space Programme 2012-2015) and GeoERA HotLime (Horizon 2020, 2018-2021) has been used. In view of data interoperability, the data model has been developed as an extension of the INSPIRE Geology data model. The dataset is served through APIs conforming to the OGC API – Feature standard and is downloadable also in GeoPackage format, in this anticipating the application of the principles established by the Open Data Directive (Directive (EU) 2019/1024) regarding the sharing of the High Value Datasets.The 3D geological model of the Padan basin includes the geometry of four boundary horizons (roof or discordance) of successions of homogeneous lithologicalmnete sedimentary units, in the Triassic – Pleistocene range, and 179 fault geometries. Each stratigraphic horizon is also described through isobates. Where possible, in addition to the absolute quota value, the value of the thickness of the succession above or below is also provided, respectively if it is a discrepancy or a roof. It also describes the lithology, geological process and age of each sedimentary succession. Each fault, with its upper edge, is accompanied by kinematics, mean values derived from 3D geometry, and by the age of the oldest and youngest faulted/deformed stratigraphic unit, if derived from the 3D geological model.This dataset and its data model were obtained as part of the GO-PEG project (https://www.go-peg.eu/), co-financed by the Connecting Europe Facility (CEF) of the European Commission. More specifically, this dataset is the output of the go-depth use case, which aims to provide a methodology and model capable of conceptualising, organising and providing easy-to-use, high-quality and interoperable subsoil information for sustainable planning and use of natural resources. For this purpose, data from the European projects GeoMol (Alpine Space Programme 2012-2015) and GeoERA HotLime (Horizon 2020, 2018-2021) were used. In order to facilitate data interoperability, the data model was developed as an extension of the INSPIRE Geology data model. The dataset is served through APIs compliant with the OGC API – Feature standard and is also downloadable in GeoPackage format, anticipating in this the application of the principles established by the Open Data Directive (Directive (EU) 2019/1024) regarding the sharing of the High Value Data Set.波河盆地（Po Basin）地质三维模型涵盖了三叠纪至更新世时间区间内，围限岩性均一沉积层序的4个地层界面（顶面或不整合面）的几何形态，以及179处断裂构造的几何形态。每个地层界面均附带其埋深等值线（isobaths）；在可行情况下，同时提供基底不整合面与顶面之上、之下的层序厚度，以及该界面的地表埋深。本数据集同时涵盖各沉积层序的岩性、地质作用过程与形成时代。每一处断裂附带其上断点线，并提供由三维地表几何形态推导得到的运动学特征、走向、倾向方位角与倾角的平均值；若可从三维地质模型中获取，则同时提供该断裂错断或变形的最老与最新地层界面的形成时代。 本数据集及其关联数据模型依托欧盟委员会欧洲互联互通设施（Connecting Europe Facility, CEF）联合资助的GO-PEG项目（https://www.go-peg.eu/）研发完成。具体而言，本数据集为go-depth应用场景的产出成果，该场景旨在构建一套方法与模型，以实现地下信息的概念化、组织与交付，为自然资源的可持续规划与利用提供易用、高质量且具备互操作性的地下数据支持。为此，本数据集整合了欧盟资助项目GeoMol（阿尔卑斯空间计划2012-2015年）与GeoERA HotLime（地平线2020计划2018-2021年）的相关数据。为保障数据互操作性，本数据模型以INSPIRE地质数据模型为基础进行扩展开发。本数据集通过符合OGC API – Feature标准的应用程序编程接口（API）提供服务，同时支持以GeoPackage格式下载，此举旨在落实《开放数据指令》（欧盟指令(EU) 2019/1024）中关于高价值数据集共享的相关原则。 帕达纳盆地（Padan basin）地质三维模型涵盖了三叠纪至更新世时间区间内，围限岩性均一沉积层序的4个边界界面（顶面或不整合面）的几何形态，以及179处断裂构造的几何形态。每个地层界面同样通过埋深等值线（isobates）进行描述；在可行情况下，除提供该界面的绝对高程值外，若为不整合面或顶面，还将分别提供其之上或之下的层序厚度。本数据集同时涵盖各沉积层序的岩性、地质作用过程与形成时代。每一处断裂附带其上断点，并提供由三维几何形态推导得到的运动学特征平均值；若可从三维地质模型中获取，则同时提供该断裂错断或变形的最老与最新地层单元的形成时代。 本数据集及其关联数据模型依托欧盟委员会欧洲互联互通设施（Connecting Europe Facility, CEF）联合资助的GO-PEG项目（https://www.go-peg.eu/）研发完成。具体而言，本数据集为go-depth应用场景的产出成果，该场景旨在构建一套方法与模型，以实现地下信息的概念化、组织与交付，为自然资源的可持续规划与利用提供易用、高质量且具备互操作性的地下数据支持。为此，本数据集整合了欧盟资助项目GeoMol（阿尔卑斯空间计划2012-2015年）与GeoERA HotLime（地平线2020计划2018-2021年）的相关数据。为保障数据互操作性，本数据模型以INSPIRE地质数据模型为基础进行扩展开发。本数据集通过符合OGC API – Feature标准的应用程序编程接口（API）提供服务，同时支持以GeoPackage格式下载，此举旨在落实《开放数据指令》（欧盟指令(EU) 2019/1024）中关于高价值数据集共享的相关原则。