• Tidak ada hasil yang ditemukan

isprs archives XLII 2 W2 63 2016

N/A
N/A
Protected

Academic year: 2017

Membagikan "isprs archives XLII 2 W2 63 2016"

Copied!
4
0
0

Teks penuh

Gambar

Figure 1. Fundamental body split by the geological interface
Figure 10. The stratum models were constructed after series of interface splitting from bounding box
Figure 11. The pinch-out stratum model was simulated very naturally and precisely

Referensi

Dokumen terkait

The implementation of 3D DHE vario-scale model starts with the basic and topological cleaned 2D dataset (validated without geometry and topological error), followed by

In this paper, we regard the point cloud registration as a stochastic system and the global registration as the process that recursively estimates the rigid transformation

This paper proposed a coded sequence pattern for automatic matching of LiDAR point data, the methods including SIFT features, Otsu segmentation and Fast

Considering the context of study (e.g. simulation model used, type of input varied), the building orientation and height were assessed as the most influential parameters

Both datasets were acquired with a combination of five cameras, IGI DigiCam in a Maltese cross configuration, with a tilt angle of 45 degrees. However, for this

Processing high resolution image sequences through SfM photogrammetry software, a 5cm pixel size orthophoto was produced and was used to identify the rolling section and the

Results show that uncertainty can vary significantly depending on the characteristics of the urban area and the granularity of the analysis (sensor, building and group of buildings).

GEOLOGICAL MAPPING OF CRATER LALANDE Our geological map contains eight geological units organized by crater floor units: hummocky floor, central peak and low- relief