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Shou Yeh Gong
Researcher at Houston Museum of Natural Science
Publications - 6
Citations - 60
Shou Yeh Gong is an academic researcher from Houston Museum of Natural Science. The author has contributed to research in topics: Carbonate & Coral reef. The author has an hindex of 4, co-authored 5 publications receiving 45 citations.
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Journal ArticleDOI
Dry climate near the Western Pacific Warm Pool: Pleistocene caliches of the Nansha Islands, South China Sea
Shou Yeh Gong,Horng Sheng Mii,Kuo-Yen Wei,Chorng Sherng Horng,Chen-Feng You,Fu Wen Huang,Wen Rong Chi,Tzen-Fu Yui,Pei Keng Torng,Shieu Tsann Huang,Shih-Wei Wang,Jong Chang Wu,Kenn Ming Yang +12 more
TL;DR: The Nansha caliche as mentioned in this paper indicates the existence of several dry climate episodes during Pleistocene sea-level lowstands, which may explain the higher sea surface salinities reported elsewhere in the South China Sea.
Journal ArticleDOI
Cold-seep carbonate hardgrounds as the initial substrata of coral reef development in a siliciclastic paleoenvironment of southwestern Taiwan
Journal ArticleDOI
Hydroclimate variability of central Indo-Pacific region during the Holocene
Sakonvan Chawchai,Liangcheng Tan,Liangcheng Tan,Ludvig Löwemark,Hao Cheng Wang,Tsai Luen Yu,Yun Chuan Chung,Horng Sheng Mii,Guangxin Liu,Maarten Blaauw,Shou Yeh Gong,Barbara Wohlfarth,Chuan-Chou Shen +12 more
TL;DR: In this article, the authors present a decadal-resolved hydroclimate record covering the past 11 thousand years based on δ18O data of three stalagmites from Klang Cave (TK) on the Thai-Malay Peninsula, southern Thailand.
Journal ArticleDOI
Hydrocarbon-derived carbonate cements of subsurface origin in the Vulcan Sub-basin, Timor Sea
Shou Yeh Gong,Horng Sheng Mii,Ming Shyan Wu,Kuo An Lin,Shih-Wei Wang,Ting Fang Chou,Ying Wei Chou,Jong Chang Wu,Yuh Ruey Wang +8 more
TL;DR: In this article, localized carbonate cements in the Eocene Grebe Sandstone of the Vulcan Sub-basin, Timor Sea, Australia were investigated and it was shown that only the cements associated with sandstones were probably hydrocarbon-derived, and the resultant mineral is mainly calcite.