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          "Souvrství Cloverly je geologické souvrství, jehož sedimenty se rozkládají na území západoamerických států Montana, Wyoming, Colorado a Utah. Své jméno odvozuje od poštovní stanice, která se na přelomu 19. a 20. století nacházela na východní straně Bighornské pánve. Jméno pro souvrství zvolil N. H. Darton v roce 1904.",
          "La formation de Cloverly est une formation géologique datant du Crétacé inférieur (Aptien et Albien) située dans les États du Montana et du Wyoming aux États-Unis.",
          "La formació de Cloverly data del Cretaci inferior i està localitzada a Montana i Wyoming, a l'oest dels Estats Units.",
          "La Formación Cloverly , es una formación geológica datada alrededor de 112 a 99,6 millones de años atrás en el Albiense durante el Cretácico inferior, en el bajo de Bighorn, en el límite entre los estados de Montana y Wyoming, en Estados Unidos, incluyendo el estrato anteriormente llamado Formación Dakota. Tiene un grueso medio de aproximadamente 90 metros y parte superior de la Fm. Cloverly es marcada por facies marinas transgresiva, depositada por un mar interior que penetro en dirección Sur Se la divide en tres miemnbros \n* El Conglomerado Pryor ubicada en la base y contienen sílex negro abundante. Se nombra de las camas gruesas expuestas en el lado oeste de las . \n* El Miembro Little Sheep Member en el centro y se compone de lutolita pálido-púrpura, gris a la casi blanca y bentonita. Una edad radiométrica de 115 +/- 10 millones de años que se ha obtenido del punto bajo en el miembro (Chen y Lubin 1997), y en el superior de 108.5 +/- 0.2 millones de años (Burton y otros 2006). Estas fechas confirman que el Cloverly es Aptiano-Albiano. \n* El Miembro Himes es el superior y contiene algunos depósitos de grano grueso de un lecho, pero compuesto sobre todo de lutolitas brillantes y multicolores." ] ,
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