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Institution

Central Geological Survey, MOEA

GovernmentTaipei, Taiwan
About: Central Geological Survey, MOEA is a government organization based out in Taipei, Taiwan. It is known for research contribution in the topics: Landslide & Fault (geology). The organization has 68 authors who have published 81 publications receiving 2037 citations. The organization is also known as: Jīngjì Bù Zhōngyāng Dìzhí Diàochá Suǒ.


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Journal ArticleDOI
TL;DR: A high-resolution 2-ky record of changes in sediment delivery to Dahu, a floodplain lake in northeastern Taiwan, that suggests changes in precipitation has been inferred from organic matter, pollen, and spores in a 12m sediment core and from the organic matter compositions of soil, catchment plants, and fluvial suspended sediment as discussed by the authors.

13 citations

Journal ArticleDOI
TL;DR: In this paper, the authors used reflection seismic data to derive geothermal gradient patterns at different sub-seafloor depths, then calculated 1D vertical fluid flow models by analyzing the Peclet numbers in the offshore regions of SW Taiwan.
Abstract: Fluid migration rates are important parameters for understanding the structural characteristics and evolu- tion of the crustal tectonics and hydrocarbon exploration. However, they are difficult to measure on the seafloor. Densely sampled temperature measurements might shed light on our study of the fluid migration rates. In this study, we first use reflection seismic data to derive geothermal gradient patterns at different sub-seafloor depths, then calculated 1D vertical fluid flow models by analyzing the Peclet numbers in the offshore regions of SW Taiwan. We found Peclet numbers ranging from 2 to 5, implying that vertical fluid flow velocities are between 6 and 44 cm/year. Assumed a homogenous permeable layer and no lateral variation of the temperature fields, we analyzed possible errors caused by depth-dependent thermal conductivity and velocity-depth function. They probably cause less than 2 cm/year of errors in the estimated vertical fluid flow rate. In terms of regional fluid flow patterns, we found higher fluid flow rates near the toe of the trench, and a dramatic increase in fluid flow rate when the continental slope of the Chinese passive margin enters into the trench, and reduced fluid flow rates in the hinterland. We propose that this is a new and potentially useful method to derive regional fluid flow rate models for studying geochemical and biological processes in shallow seafloor sediments and the regional hydrological budget.

12 citations

Journal ArticleDOI
TL;DR: In this article, the authors developed a methodological framework to analyze the susceptibility of layered rock slopes from regional to local scales, where the appropriate size of the slope unit (SU) was produced as the mapping unit through the object-based image analysis (OBIA) method, and the susceptibility map was generated with an explicit purpose according to the resolution of geological data.

12 citations

Journal ArticleDOI
TL;DR: In this paper, the Tunglo Fault System (TFS) was found in the fold and thrust belt between Tung Lo town and the Tachia River in northwestern Taiwan, which formed after the area's oldest fluvial terrace and appears at least 16km long in roughly N-S orientation.

12 citations

Journal ArticleDOI
TL;DR: In this article, the Oligo-Miocene coastal-shelf strata of a mid-Tertiary rift basin in Taiwan were identified and correlated regionally, constrained by microfossil biohorizons and radioactive dates.

12 citations


Authors
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Performance
Metrics
No. of papers from the Institution in previous years
YearPapers
20231
20211
20205
20194
20184
20178