C
Chia-Yu Lu
Researcher at National Taiwan University
Publications - 49
Citations - 1686
Chia-Yu Lu is an academic researcher from National Taiwan University. The author has contributed to research in topics: Subduction & Collision zone. The author has an hindex of 17, co-authored 48 publications receiving 1484 citations. Previous affiliations of Chia-Yu Lu include Adept Technology.
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Preliminary neotectonic map of onshore-offshore Taiwan
Benoît Deffontaines,Char-Shine Liu,J. Angelier,Chyi Tyi Lee,Jean-Claude Sibuet,Yi-Ben Tsai,Serge Lallemand,Chia-Yu Lu,Chao Shing Lee,Shu Kun Hsu,Hao-Tsu Chu,Jian-Cheng Lee,Erwan Pathier,Rou-Fei Chen,Chin-Tung Cheng,Chi-Wen Cheng,C-W L +16 more
TL;DR: In this paper, a multisource approach has been applied to data sets both onland and offshore Taiwan, and has resulted in a preliminary neotectonic map of onshore-offshore Taiwan.
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Nappe structure revealed by thermal constraints in the Taiwan metamorphic belt
TL;DR: In this article, the authors used Raman spectroscopy of carbonaceous material data to better resolve the thermal history of the Hsuehshan Range, which is accreted between the foreland fold-thrust belt and bulldozer hinterland units in the Taiwan mountain belt.
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Energy control by linking individual patterns to self-repeating diffractive optical elements
TL;DR: It was found that adding the preserving-the-best strategy to traditional genetic algorithms guarantees the possibility of locating the global optimum and makes this newly developed genetic algorithm an effective method for designing diffractive optical elements.
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Growth Normal Faulting at the Western Edge of the Metropolitan Taipei Basin since the Last Glacial Maximum, Northern Taiwan
TL;DR: In this paper, the authors present the Shanchiao Fault as a case study which is an active normal fault responsible for the formation of the 700-m-thick late Quaternary deposits in Taipei Basin at the northern tip of the Taiwan mountain belt.
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Elucidating the geometry of the active Shanchiao Fault in the Taipei metropolis, northern Taiwan, and the reactivation relationship with preexisting orogen structures
TL;DR: In this paper, a 2D profile across the Shanchiao Fault is chosen for elastic half-space dislocation modeling, and the results suggest that the fault is listric in the shallow crust with an abrupt change from subvertical ramp (85°-75°) to near-horizontal flat (10°-15°) at 3-4 km depth, consistent with an origin from the inversion of an orogen-related thrust detachment.