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Final Map xsection bd LinkedIn
- 1. Height(m) 1000 2000 30004000 Distance (m) 1100 1000 1200 1300 1400 1500 1600 1700 1800 1900 2000 2100 2200 2300 1100 1000 1200 1300 1400 1500 1600 1700 1800 1900 2000 2100 2200 2300 NESW CSF PLF ACFCCF UMF CLF ACF CLF UMF PLF CSF BedThickness(m) 1300 1350 1250 1250 1200 1300 1250 1300 1300 1350 1300 1100m 1200m 1150m 1250m 1300m 1350m 1100m 1200m 1150m 1250m 1300m 1350m 1000 900 800 700 600 500 400 300 200 100 0 CSF PLF UMF CLF ACF CCF Camarillas Sandstone Formation Medium to coarse calcareous sand. Bed thickness ranged from 30cm to 200cm. Contained mostly CaCO3 and small shell fragments. Redish tint is iron oxide staining. Overall thickness undetermined because there is no exposure of basal contact on the surface. Palomar Limestone Formation Transition between competent and incompetent bedding. Consist of about 60-70% carbonate mud throughout all its members, with more and more fossil evidence towards the Upper Palomar Member and the overlying lithology. Bed thickness ranges from 50cm - 200cm Utrillas Marl Formation The Utrillas Marl Formation is a series of interbedded competent white carbonate sands and less competent carbonate-rich mudstone. Bed thickness ranges from 20cm to 200cm. Contains coal seams and gypsum crystals. Canadillas Limestone Formation Interbedded mircritic limestone with angular clasts. Bed thickness is 50cm to >100cm. Dogtooth calcite is present in fabric. A small section of this formation has been slightly dolomitised, but not seen in the area of study. Aldehuela Conglomerate Formation Has rounded clasts embedded in a sandy matrix. 75% of the clasts are micritic limestone. Undetermined bed thickness and estimated overall thickness of 200m. Represents an erosional surface overlying an angular unconformity. Covachuela Conglomerate Formation Contains a poorly sorted matrix of sand and 50cm+ clasts. This unit represents an unconformable erosional surface. Also shows upward fining. The Geology of Aliaga, North Spain By Gabriel W. Clemente 2014 08 21 35 30 54 32 22 20 28 52 30 67 62 62 77 74 1262 3740 20 35 40 42 20 40 62 70 60 61 1362 60 62 1307 21 30 20 30 44 80 1352 1372 1335 1367 1335 1376 1368 1381 70 135570 60 1398 1381 60 70 60 1249 1254 1277 1265 1361 Las Calzadas Cabezo Agudo El Reguero El Colladillo Cabezo Navarro El Campo Cabezo de Cerrado Alto Las Penuelas El Plano La Hoya Loma de San Martin Pinarolo Campos Hoya Caoilla 1422 Cerrode las Aceras Fuente Serval La Rinconada Las Clochas Cabezo del Collado del Pino Minas delSalobral (Abandonadas) La Covachuela Loma del Molar Loma del Horcajo Los Arbellonas La Fuenfresca Hoya del Campo 1200 12501300 1250 1414 1346 1323 1313 1319 1341 1216 1232 1233 1253 1247 Guadalope 691 692 693 694 510 510 509 509 508 508 507 507 506 507 691 692 693 694 Thrust Fault - Teeth point to block that has been thrusted Inferred Boundary Direct Contact Between both Formations Unconformity Structural Symbols Strike & Dip Horizontal Bed Overturned Bed Inferred Fault Clear Normal Fault 1352 Spot Height Anticline Axial Trace Syncline Axial Trace Younging Direction Sedimentary Symbols Shell Fragments Brachiopod Fossilised Coral Gastropod Oysters Numelites Other Mapping Symbols Locality Number Outcrop Cross-Bedding Upward Grading Buildings/Ruins Abondoned Mines X X1 X X1 Gypsum Crystals } LowerCretaceous } UpperCretaceous } TERTIARY 1 TNMD MD Magnetic Declination TN True North