PPT-Interpreting detrital zircon provenance in the context of regional stratigraphic and tectonic

Interpreting detrital zircon provenance in the context of regional stratigraphic and tectonic models an example from Late OrdovicianEarly Devonian cover rocks on Ganderia eastern Maine Allan Ludman John Aleinikoff Bill Devlin. U.S. Department of the InteriorBruce Babbitt, SecretaryU.S. Geological SurveyCharles G. Groat, DirectorFor sale by U.S. Geological Survey, Information ServicesBox 25286, Federal CenterDenver, CO 8022 Stratigraphy. B. Natalin. 2. Prof. Dr. Boris . Alekseevich. Natalin, . Office – E 502. Phone – 285 6221, . e-mail: . natalin@itu.edu.tr . Website: . http://web.itu.edu.tr/~natalin/. . Assistant: Ali . UNIT . 5. What are Sediments. Sediments are loose Earth materials (unconsolidated materials) such as sand . which are . transported by the action of water, wind, glacial ice and . gravity.. These . materials are . The Paleozoic Era. Part 4b: . Stratigraphy. and Tectonics of Silurian and Devonian . Periods. Major Concepts. The proliferation of coral reefs caused restricted basins wherein great thickness of limestone and . -Ta and Ti in arc . magmatism:. . A . case study of the Yangzhuang granite porphyry . in . West Junggar, . Xinjiang. , China. Wei Mao. 1, 2. , Xiaofeng Li. 1. , Brian Rusk. 2. 1. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550002, China. Midterm 2. Preparation/Review. Style of Questions. Matching term w/ definition. Short definition of concepts/processes. Name some of multiple characteristics. 25% of points from Part II Quizzes. REVIEW . What’s changing…and what’s remaining the same. Maine Libraries Conference – November 2016. October 1973…. The Maine Regional Library System . 2. .. Three districts. …. Three consultants…. Xianghui Li. 1. , Frank Mattern. 2. , Chaokai Zhang. 1. , Qinggao Zeng. 3. , Guozheng Mao. 3. . 1School. of Earth Sciences and Engineering, Nanjing University, Nanjing, 210046, China. Email: . leeschhui@126.com. What are Sediments. Sediments are loose Earth materials (unconsolidated materials) such as sand . which are . transported by the action of water, wind, glacial ice and . gravity.. These . materials are . lithostratigraphy. GEOLOGICAL TIME. The passage of time since the formation of the . Earth is . divided into . geochronological. . units. .. T. hese are divisions . of time that may . be referred . to in terms . SEDIMENTARY ROCKS. Geo 281: geology for engineers. Geology and Geophysics Department. King Saud University. What are Sediments. Sediments are loose Earth materials (unconsolidated materials) such as sand . By. Dr. Muhamed F. Omer. Post-doctoral . /. Warsaw University 2014. Salahaddin University- Science College, Geology Department . Iraqi Kurdistan Region-Erbil. muhfakhri2005@ gmail.com. Tel. 009647701348322. Trexler. et al., 2004. Background. Orogenies. in the Paleozoic in western North America have traditionally been grouped into two:. Late-Devonian through Early Mississippian Antler Orogeny. Late Permian-Early Triassic Sonoma Orogeny. Mahyra Tedeschi. 1*. , . Humberto Reis. 2. , Laura Stutenbecker. 3. , Matheus Kuchenbecker. 4. , Bruno Ribeiro. 5. ,. . Vitor Barrote. 6. , Pedro Leonardo Vieira. 1. , Cristiano Lana. 2. 1. Universidade Federal de Minas Gerais, .