Moonsoo Shin

ORCID: 0000-0002-3115-3670
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About
Contact & Profiles
Research Areas
  • Geological formations and processes
  • Hydrocarbon exploration and reservoir analysis
  • Hydraulic Fracturing and Reservoir Analysis
  • Geological Modeling and Analysis
  • Forensic Anthropology and Bioarchaeology Studies
  • Health and Medical Education
  • Chromosomal and Genetic Variations
  • Geology and Paleoclimatology Research
  • Seismic Imaging and Inversion Techniques
  • Botany and Geology in Latin America and Caribbean
  • Plant Disease Resistance and Genetics
  • Plant Molecular Biology Research

The University of Texas at Austin
2019-2020

Korea Post
2005

Pohang University of Science and Technology
2005

We have generated 47,932 T-DNA tag lines in japonica rice using activation-tagging vectors that contain tetramerized 35S enhancer sequences. To facilitate use of those lines, we isolated the genomic sequences flanking inserted via inverse polymerase chain reaction. For most performed four sets amplifications two different restriction enzymes toward both directions. In analyzing 41,234 obtained 27,621 sequence tags (FSTs), among which 12,505 were integrated into genic regions and 15,116...

10.1111/j.1365-313x.2005.02610.x article EN The Plant Journal 2005-12-05

Abstract Coarse‐grained turbidite systems have been broadly described mostly on tectonically active basins, but there is lack of a detailed depositional and facies model in relatively unconfined settings. A large outcrop the Los Molles Formation Neuquen Basin used to build architecture, hierarchy distribution coarse‐grained system. high‐resolution satellite image, drone imagery 4000 m deposits measured 20 locations with description are isopach net gross maps that allowed reconstruction The...

10.1111/sed.12771 article EN Sedimentology 2020-06-10

Abstract Seismic‐reflection data show that most deepwater (>200 m water depth) basins are filled by sand and mud dispersed across clinoformal geometries characterized gently dipping topsets, steeper foresets bottomsets. However, the entire geometry of these ubiquitous clinoforms is not always recognized in outcrops. Sometimes infill erroneously interpreted as “layer cake” or “ramp” stratigraphy because topset‐foreset‐bottomset well exposed. Regional 2‐D seismic lines Lower to Middle...

10.1111/bre.12395 article EN Basin Research 2019-09-03
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