Josep Anton Muñoz
Biographic Data
| ID | 8536995 |
|---|---|
| NAME | Josep Anton Muñoz |
| GIVEN NAMES | Josep Anton |
| FAMILY NAME | Muñoz |
| SIGNATURE | MUÑOZ J A |
| AFFILIATIONS | Universitat de Barcelona |
| ORCID | 0000-0003-0740-879X |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 5 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2016 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 0 |
From scientific research to digital reconstruction
There is a lack of bibliography concerning the specific methodology and limitations of historical data gathering to achieve high-quality and accurate productions of virtual reality (VR) and augmented reality (AR) technology applied to heritage dissemination. Most papers focus on the technical features and dissemination application of 3D and VR; the rigour of the research process specifically aimed at 3D reconstruction is usually not addressed, or…
Surface and subsurface geology of the Hontomín structure, Western Pyrenees
A detailed geological study was conducted in the Hontomín area in the western Pyrenees, Northern Spain, focusing on structural characterization by integrating available subsurface data with a newly developed surface geological map. It reveals a relatively simple surface structure, with the Upper Cretaceous generally dipping gently eastward, except at the southern margin, where they are deformed into tight E-W-trending folds. In contrast, the unco…
Geology of the eastern tip of the El Tordell Fault, Southern Pyrenees
Along strike variations of frontal structures at fold and thrust belts allow us deciphering the evolution of contractional structures at early stages of deformation but also, how processes such as salt mobilisation, thrust emplacement, and folding develop. The external parts of the Pyrenees are suitable to investigate how these processes interacted during the Pyrenean Orogeny. The integration of fieldwork and subsurface data allowed us to obtain …
Geology of the Golobar and Rumaceo faults, Basque-Cantabrian Pyrenees
The lateral transition between different styles of deformation is crucial for understanding local-scale structures since it influences orogenic reconstructions at the crustal scale. This is especially important at the westernmost Basque-Cantabrian Pyrenees, where the transition from the thin-skinned Basque-Cantabrian Pyrenees to the thick-skinned Cantabrian Mountains remains a subject of debate. To address this, detailed geological mapping and pr…
Geology of the Cotiella thrust sheet, southern Pyrenees (Spain)
This paper presents a geological map and cross-sections of the Cotiella thrust sheet at 1:25,000 and 1:50,000 scale, respectively. The map covers an area of 225 km2 in the southern Pyrenees. The structure of the studied area is dominated by an upper Santonian – lower Miocene thrust system, which transported a middle Coniacian-lower Santonian extensional basin, the Cotiella Basin, 10 s of kilometres southwards during the Pyrenean orogeny. The map …
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Geology of the Cotiella thrust sheet, southern Pyrenees (Spain)
This paper presents a geological map and cross-sections of the Cotiella thrust sheet at 1:25,000 and 1:50,000 scale, respectively. The map covers an area of 225 km2 in the southern Pyrenees. The structure of the studied area is dominated by an upper Santonian – lower Miocene thrust system, which transported a middle Coniacian-lower Santonian extensional basin, the Cotiella Basin, 10 s of kilometres southwards during the Pyrenean orogeny. The map …
Geology of the eastern tip of the El Tordell Fault, Southern Pyrenees
Along strike variations of frontal structures at fold and thrust belts allow us deciphering the evolution of contractional structures at early stages of deformation but also, how processes such as salt mobilisation, thrust emplacement, and folding develop. The external parts of the Pyrenees are suitable to investigate how these processes interacted during the Pyrenean Orogeny. The integration of fieldwork and subsurface data allowed us to obtain …
Geology of the Golobar and Rumaceo faults, Basque-Cantabrian Pyrenees
The lateral transition between different styles of deformation is crucial for understanding local-scale structures since it influences orogenic reconstructions at the crustal scale. This is especially important at the westernmost Basque-Cantabrian Pyrenees, where the transition from the thin-skinned Basque-Cantabrian Pyrenees to the thick-skinned Cantabrian Mountains remains a subject of debate. To address this, detailed geological mapping and pr…
From scientific research to digital reconstruction
There is a lack of bibliography concerning the specific methodology and limitations of historical data gathering to achieve high-quality and accurate productions of virtual reality (VR) and augmented reality (AR) technology applied to heritage dissemination. Most papers focus on the technical features and dissemination application of 3D and VR; the rigour of the research process specifically aimed at 3D reconstruction is usually not addressed, or…
Surface and subsurface geology of the Hontomín structure, Western Pyrenees
A detailed geological study was conducted in the Hontomín area in the western Pyrenees, Northern Spain, focusing on structural characterization by integrating available subsurface data with a newly developed surface geological map. It reveals a relatively simple surface structure, with the Upper Cretaceous generally dipping gently eastward, except at the southern margin, where they are deformed into tight E-W-trending folds. In contrast, the unco…
Geological and Geophysical Studies Worldwide (4 works) · Geology (4 works) · Geomorphology (4 works) · Geological and Geochemical Analysis (3 works) · Geologic map (2 works) · Geological formations and processes (2 works) · Seismology (2 works) · 3D Surveying and Cultural Heritage (1 works) · Archaeology (1 works) · Augmented reality (1 works)