Abstract

This paper demonstrates an integrative 3D model of short-wave infrared (SWIR) hyperspectral mapping and unmanned aerial vehicle (UAV)-based digital elevation model (DEM) for a carbonate rock outcrop including limestone and dolostone in a field condition. The spectral characteristics in the target outcrop showed the limestone well coincided with the reference spectra, while the dolostone did not show clear absorption features compared to the reference spectra, indicating a mixture of clay minerals. The spectral indices based on SWIR hyperspectral images were derived for limestone and dolostone using aluminum hydroxide (AlOH), hydroxide (OH), iron hydroxide (FeOH), magnesium hydroxide (MgOH) and carbonate ion (CO32−) absorption features based on random forest and logistic regression models with an accuracy over 87%. Given that the indices were derived from field data with consideration of commonly occurring geological units, the indices have better applicability for real world cases. The integrative 3D geological model developed by co-registration between hyperspectral map and UAV-based DEM using best matching SIFT descriptor pairs showed the 3D rock formations between limestone and dolostone. Moreover, additional geological information of the outcrop was extracted including thickness, slope, rock classification, strike, and dip.

Highlights

  • IntroductionSedimentary rocks, one of the three major rock types, are one of the most widely distributed rocks on Earth’s surface covering 66% [1]

  • A carbonate rock outcrop composed of alternative layers of limestone and dolostone was scanned with a short-wave infrared (SWIR) hyperspectral imaging system and classified with an random forest (RF) algorithm to derive spectral bands sensitive to mapping of carbonate rocks for constructing logistic regression models

  • A digital elevation model (DEM) and ortho-rectified images were generated by the SfM algorithm from unmanned aerial vehicle (UAV) images

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Summary

Introduction

Sedimentary rocks, one of the three major rock types, are one of the most widely distributed rocks on Earth’s surface covering 66% [1]. They are mainly produced in a water environment such as an ocean basin as a sedimentation originated from weathering, erosion, and transportation of continental rocks. The main components describing the sedimentary rocks are lithology, thickness, strike, and dip of bedding planes. Lithology and thickness describe the characteristics of environment and duration of sedimentation. Strike and dip depict how a sedimentary layer is positioned and its inference of the history of

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