final map xsection bd linkedin

1
Height (m) 1000 2000 3000 4000 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 NE SW CSF PLF ACF CCF UMF CLF ACF CLF UMF PLF CSF Bed Thickness (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 37 40 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 1355 70 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 12 50 1300 1 250 1414 1346 1323 1313 1319 1341 1216 1232 1233 1253 1247 G uadalo pe 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 } Lower Cretaceous } Upper Cretaceous } TERTIARY 1 TN MD MD Magnetic Declination TN True North

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Page 1: Final Map xsection bd LinkedIn

He

igh

t (m)

1000 2000 3000 4000

Distance (m)

1100

1000

1200

1300

1400

1500

1600

1700

1800

1900

2000

2100

2200

2300

1100

1000

1200

1300

1400

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1900

2000

2100

2200

2300 NESW

CSFPLF

ACFCCF UMF CLF

ACF

CLF

UMF

PLF

CSF

Be

d T

hick

ne

ss (m)

1300

1350

1250

1250

1200

1300

12501300

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 FormationMedium 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 FormationTransition between competent and incompetent bedding. Consist of about 60-70% carbonate mud throughoutall 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 FormationThe 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 FormationInterbedded 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 FormationHas 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 anangular unconformity.

Covachuela Conglomerate FormationContains a poorly sorted matrix of sand and 50cm+ clasts. This unit represents an unconformable erosional surface. Also shows upward �ning.

The Geology of Aliaga, North SpainBy

Gabriel W. Clemente2014

08

21

35

30

54

3222

2028 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

PinaroloCampos

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

12001250

13001250

1414

1346

1323

13131319

1341

1216

1232

1233 1253

1247

Guada

lope

691

692693

694

510510

509509

508508

507507

506507

691

692

693694

Thrust Fault - Teeth point to block that has been thrusted

Inferred Boundary

Direct Contact Between bothFormations

Unconformity

Structural Symbols

Strike & Dip

Horizontal Bed

Overturned Bed

Inferred Fault

Clear Normal Fault

1352 Spot Height

Anticline AxialTrace

Syncline Axial Trace

Younging Direction

Sedimentary Symbols

Shell Fragments

Brachiopod

Fossilised Coral

Gastropod

Oysters

Numelites

Other Mapping SymbolsLocality Number

Outcrop

Cross-Bedding

UpwardGrading

Buildings/Ruins

Abondoned Mines

X

X1

X X1

Gypsum Crystals

}

Lower Cretaceous

}Upper Cretaceous

}

TERTIARY

1

TNMD

MD Magnetic Declination

TN True North