Subsurface Structure Investigation from High-Resolution Seismic Reflection Data

Subsurface Structure Investigation of the Longitudinal Valley, Eastern Taiwan from High-Resolution Seismic Reflection Data

  1. The profile J north of the Peinanshan in Luyeh reveals the east-dipping Luyeh fault, and the undulations of the alluvium strata are observed as a result of the fault.

  2. The deformation and tilting of the sedimentary strata in the southern Longitudinal Valley is inferred to relate to the collision toward the northwest from the southern Costal Range and the reverse movement of active faults in the LV.

賴思穎 Szu-Ying Lai
碩士論文:應用高解析反射震測探討花東縱谷地下構造
Master’s Thesis: Subsurface Structure Investigation of the Longitudinal Valley, Eastern Taiwan from High-Resolution Seismic Reflection Data

Seismic reflection survey in eastern Taiwan

Seismic reflection survey in the northern part of the Longitudinal Valley, the suture zone, in eastern Taiwan

  1. In this study, we found that beneath the longitudinal valley, there are about 2000 m thick of sedimentary beddings laid on top of the basement dipping to the east.

  2. In fact that only Lingding fault has been found in the section, no other major fault has been discovered.

謝一銘 Yi-Ming Shie
碩士論文:台灣花東縱谷北段反射震測調查
Master’s Thesis: Seismic reflection survey in the northern part of the Longitudinal Valley, the suture zone, in eastern Taiwan

Study seismic stratigraphy in the alluvium fan

Study seismic stratigraphy in the alluvium fan

  1. We have completed four seismic profiles with a total of 10.748 km in length and according to the seismic data four unconformities can be identified from seismic stratigraphy analysis.

  2. According to the analysis of sequence stratigraphy, it is found that this area is in a sedimentary cycle from the development of the transgressive system to the high stand system tracts, and from the topographies of the unconformities in different periods it indicates that the river was through headward erosion.

Improving the seismic imaging by using multiple attenuation methods

Improving the seismic imaging in the southern Ryukyu subduction system by using multiple attenuation methods

  1. In this study, we test two sets of multiple attenuation methods: differentiate the physical properties and modeling multiples from sea bed and signal.

  2. We end up using the flow: surface related multiple elimination(SRME), Radon transform, dip-filter and deconvolution.

呂奇祝 Ci-Jhu Lyu
碩士論文:利用複反射衰減方法提高海上震測成像並探討南琉球隱沒系統
Master’s Thesis: Improving the seismic imaging in the southern Ryukyu subduction system by using multiple attenuation methods

Fault Investigation Using Shallow Seismic Survey

Yuli Fault Investigation Using Shallow Seismic Survey

  1. In this study, we combine two types of active source for fault imaging: Minivibe and weight drop.

  2. The reflection signal from weight drop can be recovered is 700 m and from Minivibe is around  2000 m.

  3. We can clearly see the Yuli fault dipping to the east.

計畫名稱:
104年度重要活動斷層構造特性調查二期─活動斷層近地表構造特性調查(1/4)
Study of the Near Surface Structure of Active Fault (1/4)

相關文章:台灣活動斷層淺部構造的地球物理調查

Reflected and refracted seismic profiles in Taiwan and southeastern China

Reflected and refracted seismic profiles in Taiwan and southeastern China

  1. Crustal structures are imaged by active-source experiments.

  2. We used both refracted and reflected phases to model the crustal structures.

  3. The crustal evolution involved the closed rift basin in Fujian and Taiwan orogen.

Kuo, Y.W., C.Y. Wang, H. Kuo-Chen *, X. Jin, H.T. Cai, J.Y. Lin, F.T. Wu, H.Y. Yen, B.S. Huang, W.T. Liang, D. Okaya, and L. Brown (2015)  Crustal structures from the Wuyi-Yunkai orogen to the Taiwan orogen: the onshore-offshore wide-angle seismic experiments of the TAIGER and ATSEE projects, Tectonophysics, doi: 10.1016/j.tecto.2015.09.014.