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Page 1: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 2: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 3: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 4: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 5: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 6: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 7: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 8: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 9: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 10: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 11: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 12: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 13: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 14: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 15: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 16: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 17: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 18: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 19: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 20: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 21: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 22: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 23: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 24: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 25: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 26: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie
Page 27: pangea.stanford.edu · a major and persistent source of siliciclastic sediments during the Cenozoic. Cretaceous carbonates, and Tertiary—Quaternary clas- tics and carbonates overlie

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