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Geology of Greece

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The Axios Zone, also known as the Vardar Zone, represents the closing of the Axios Ocean and separates the Pelagonian zone from the Serbo-Macedonian Massif. Clastic sediments from the Paleozoic and Mesozoic ophiolites and sediments are common. Geologists subdivide it into the calc-schists, granite,
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and ophiolite of the Paeonias subzone and the acidic volcanic rocks and limestone of the Triassic-Jurassic Paikon subzone (an old island arc). The silicified ophiolites of the Almopias subzone, bordering the Pelagonian zone to the northeast represents an old
351:. Volcanoes in western Thrace, Limnos and Samothrace are on the edge of the Rhodope Massif, while the Aegean volcanic arc borders the Menderes Massif and Attico-Cycladic Massif. The Neogene Santorini volcanoes erupted in the 281:
deposited in the Triassic, together with bauxite and an ophiolite nappe was thrust to the west. Cretaceous limestones are the top unit, the Zone of Eastern Greece is overthrust onto external zones (which appear as tectonic
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is found on Kimolos and Milos and is often converted for higher swelling capacity by treating with sodium carbonate. Greece is the second largest bentonite producer after the United States.
411:: Common in hydrothermal deposits and widely exported from the island of Mykonos for oil drilling. Also found on Kos and Polyvos with total reserves of several million tons. 447:: The Chalkidiki Peninsula has 15 million tons of copper. Pyrite is common near East Peloponesus and disseminated copper sulfides are common in veins in Western Macedonia. 277:: Parts of the Pelagonian Zone are covered by Cretaceous metamorphosed rocks. Paleozoic rocks include conglomerate, sandstone, siltstone, tuff and limestone. Carbonate 583: 95: 172: 207: 142: 379:
water invaded during the Middle Pleistocene, although for the most part, the islands and water area of the Aegean did not change the during the ice ages.
200: 161: 91: 477:. Onshore oil exploration began in 1938 and moved offshore in 1970. The Prinos Anticline offshore was found to contain oil under Miocene rocks. 312:
sediment deposited after the Alpine cycle outcrops widely. The Mesohellene Trough, Epirus-Akarnania basin and Cycladic Basin are all examples of
203:. Normal faults with four kilometers of displacement are not uncommon although folding is limited—tectonic activity picked up in the Oligocene. 150: 320:. The Ionian Islands basin is part of the Preapulian Zone and may only have had an interruption in sedimentation in the late Miocene into the 134: 340:, arc fracturing brought subsidence of the Cretan Basin. Inland basins preserved numerous mammal fossils such as the Pikermi site north of 103: 610: 441:. Near Vourinos is a deposit with 1.5 million tons of ore and an ancient mine in Thessalia extracted 500,000 tons by the 1990s. 417:: Greece has over 1000 deposits particularly in the east-central part of the country, typically between limestone formations. 336:
times, the uplift of the Pindus Cordillera caused nappe formations to slide onto metamorphic rocks of the Cyclades. In the
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E. Louvari: The Cephalonia Transform Fault and its extension to western Lefkada Island (Greece). Tectonophysics 8 (1999).
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of its component unit—the Malliakos Series—has been used to infer the extension of the Olonos-Pindus Zone.
359:. Interior basins hold thick lakebed sediments from the Quaternary, indicating oscillation between cold 982: 951: 903: 800: 795: 603: 20:
is highly structurally complex due to its position at the junction between the European and African
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basin is filled with continental sediments. As the molasse basins filled during
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is the Serbo-Macedonian Massif, covering the Chalkidiki Peninsula with thick
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is found in Thrace and Macedonia, as well as in Devonian argillite veins on
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Internal zones span between the Serbo-Macedonian Massif and external zones:
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springs often preserve more recent fossil assemblages. Near
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130 kilometers north of Athens with 200 million tons of ore
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Volcanic activity in the Aegean began in the Neogene and
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Encyclopedia of European & Asian Regional Geology
241:: This zone includes metamorphosed rocks in Western 90:
are situated between the European hinterland in the
153:. Extensional faults were reactivated during the 974: 544: 532: 520: 508: 493: 187:indicate a dry time in the Eocene and Oligocene 563:A Geological Companion to Greece and the Aegean 160:. The Ionian Zone is thrust westward over the 149:, extensive block faulting differentiated the 28:Geologic history, stratigraphy & tectonics 604: 265:limestone, brecciated limestone and Triassic 191:unconformably overlies older carbonates. The 494:Moores, E.M.; Fairbridge, Rhodes W. (1997). 382: 611: 597: 473:well at Limin Keri on the southern end of 199:regions of the zone are overthrust on the 423:: Several million tons of calcium-type 305:Cenozoic (66 million years ago-present) 975: 78:and gneiss, with granite intrusions. 40:and are usually metamorphosed with no 618: 592: 560:Higgins, MD and Higgins, RA, 1996,* 13: 554: 183:and much of the western mainland. 137:spans much of western Greece with 106:, encompassing the islands in the 14: 994: 577: 229: 257:with an overlying Paleozoic and 141:evaporites overlain by Jurassic 98:and northern fore-region of the 461: 81: 487: 222:trough, with clastic Triassic 1: 498:. Springer. pp. 303–310. 480: 286: 261:nappe. The schist-sandstone, 102:. External zones include the 545:Moores & Fairbridge 1997 533:Moores & Fairbridge 1997 521:Moores & Fairbridge 1997 509:Moores & Fairbridge 1997 55:, with comparatively recent 32:Some of the oldest rocks in 7: 10: 999: 566:Cornell University Press. 226:and the Drymos Limestone. 922: 884: 626: 383:Natural resource geology 96:Serbo-Macedonian Massif 669:Bosnia and Herzegovina 357:Mycenaean civilization 316:basins from the early 275:Zone of Eastern Greece 344:in continental clay. 173:Gavrovo-Tripolis Zone 885:States with limited 535:, pp. 310–312. 523:, pp. 309–310. 511:, pp. 304–307. 363:conditions and wet 620:Geology of Europe 208:Olonos-Pindus Zone 206:Additionally, the 181:Dodecanese islands 143:neritic limestones 983:Geology of Greece 970: 969: 437:, ophiolites and 355:, destroying the 110:with dolomitized 88:sedimentary rocks 18:geology of Greece 990: 923:Dependencies and 627:Sovereign states 613: 606: 599: 590: 589: 548: 542: 536: 530: 524: 518: 512: 506: 500: 499: 491: 475:Zakynthos Island 201:Plattenkalk unit 164:and overlain by 998: 997: 993: 992: 991: 989: 988: 987: 973: 972: 971: 966: 924: 918: 904:Northern Cyprus 886: 880: 801:North Macedonia 622: 617: 580: 557: 555:Further reading 552: 551: 543: 539: 531: 527: 519: 515: 507: 503: 492: 488: 483: 464: 385: 307: 289: 239:Pelagonian Zone 232: 162:Preapulian Zone 84: 72:Strymonas River 30: 22:tectonic plates 12: 11: 5: 996: 986: 985: 968: 967: 965: 964: 959: 954: 949: 944: 939: 934: 928: 926: 925:other entities 920: 919: 917: 916: 911: 906: 901: 896: 890: 888: 882: 881: 879: 878: 876:United Kingdom 873: 868: 863: 858: 853: 848: 843: 838: 833: 828: 823: 818: 813: 808: 803: 798: 793: 788: 783: 778: 773: 768: 763: 758: 753: 748: 743: 741: 736: 731: 726: 721: 716: 711: 706: 701: 696: 691: 689:Czech Republic 686: 681: 676: 671: 666: 661: 656: 651: 646: 641: 636: 630: 628: 624: 623: 616: 615: 608: 601: 593: 587: 586: 579: 578:External links 576: 575: 574: 556: 553: 550: 549: 547:, p. 315. 537: 525: 513: 501: 485: 484: 482: 479: 463: 460: 459: 458: 448: 442: 428: 418: 412: 406: 392: 384: 381: 326:Aegean Islands 306: 303: 288: 285: 284: 283: 271: 270: 231: 230:Internal zones 228: 218:and is a deep 158:Alpine orogeny 92:Rhodope Massif 83: 80: 70:. West of the 29: 26: 9: 6: 4: 3: 2: 995: 984: 981: 980: 978: 963: 960: 958: 955: 953: 950: 948: 945: 943: 940: 938: 937:Faroe Islands 935: 933: 930: 929: 927: 921: 915: 912: 910: 909:South Ossetia 907: 905: 902: 900: 897: 895: 892: 891: 889: 883: 877: 874: 872: 869: 867: 864: 862: 859: 857: 854: 852: 849: 847: 844: 842: 839: 837: 834: 832: 829: 827: 824: 822: 819: 817: 814: 812: 809: 807: 804: 802: 799: 797: 794: 792: 789: 787: 784: 782: 779: 777: 774: 772: 769: 767: 764: 762: 761:Liechtenstein 759: 757: 754: 752: 749: 747: 744: 742: 740: 737: 735: 732: 730: 727: 725: 722: 720: 717: 715: 712: 710: 707: 705: 702: 700: 697: 695: 692: 690: 687: 685: 682: 680: 677: 675: 672: 670: 667: 665: 662: 660: 657: 655: 652: 650: 647: 645: 642: 640: 637: 635: 632: 631: 629: 625: 621: 614: 609: 607: 602: 600: 595: 594: 591: 585: 582: 581: 573: 572:0-8014-3337-1 569: 565: 564: 559: 558: 546: 541: 534: 529: 522: 517: 510: 505: 497: 490: 486: 478: 476: 472: 469:recognized a 468: 456: 452: 449: 446: 443: 440: 436: 432: 429: 426: 422: 419: 416: 413: 410: 407: 404: 400: 396: 393: 390: 387: 386: 380: 378: 374: 370: 366: 365:interglacials 362: 358: 354: 350: 345: 343: 339: 335: 331: 327: 323: 319: 315: 311: 302: 300: 295: 280: 276: 273: 272: 268: 264: 260: 256: 252: 248: 244: 240: 237: 236: 235: 227: 225: 221: 217: 213: 210:extends from 209: 204: 202: 198: 194: 190: 186: 182: 178: 174: 169: 167: 163: 159: 156: 152: 148: 145:. During the 144: 140: 136: 132: 128: 125: 121: 117: 113: 109: 105: 101: 100:African plate 97: 93: 89: 86:Alpine cycle 79: 77: 73: 69: 65: 61: 58: 54: 50: 47: 43: 39: 36:are from the 35: 25: 23: 19: 914:Transnistria 723: 562: 540: 528: 516: 504: 495: 489: 465: 462:Hydrocarbons 433:: Hosted in 346: 308: 299:ocean trench 290: 274: 238: 233: 205: 193:Peloponnesus 170: 151:Ionian Basin 85: 82:Alpine cycle 31: 17: 15: 952:Isle of Man 887:recognition 861:Switzerland 796:Netherlands 375:, brackish 330:Burdigalian 135:Ionian Zone 46:amphibolite 831:San Marino 791:Montenegro 771:Luxembourg 751:Kazakhstan 654:Azerbaijan 481:References 435:peridotite 369:Travertine 349:Quaternary 287:Axios Zone 220:allochthon 212:Montenegro 175:underlies 120:Cretaceous 108:Ionian Sea 60:intrusions 942:Gibraltar 766:Lithuania 467:Herodotus 425:bentonite 421:Bentonite 377:Black Sea 338:Tortonian 292:diabase, 282:windows). 243:Macedonia 224:sandstone 114:from the 112:limestone 104:Paxi Zone 64:Oligocene 62:from the 38:Paleozoic 977:Category 962:Svalbard 947:Guernsey 894:Abkhazia 846:Slovenia 841:Slovakia 816:Portugal 674:Bulgaria 455:laterite 431:Chromite 399:Stibnite 395:Antimony 389:Asbestos 353:Holocene 334:Langhian 322:Pliocene 267:dolomite 259:Mesozoic 255:Cyclades 247:Thessaly 185:Bauxites 168:facies. 147:Toarcian 139:Triassic 116:Jurassic 871:Ukraine 821:Romania 781:Moldova 739:Ireland 734:Iceland 729:Hungary 719:Germany 714:Georgia 704:Finland 699:Estonia 694:Denmark 679:Croatia 664:Belgium 659:Belarus 649:Austria 644:Armenia 639:Andorra 634:Albania 471:bitumen 415:Bauxite 373:Corinth 318:Miocene 314:molasse 310:Neogene 263:Permian 166:molasse 124:Miocene 68:Miocene 57:granite 42:fossils 957:Jersey 899:Kosovo 866:Turkey 856:Sweden 836:Serbia 826:Russia 811:Poland 806:Norway 786:Monaco 756:Latvia 724:Greece 709:France 684:Cyprus 570:  445:Copper 439:dunite 409:Barite 405:island 361:desert 342:Athens 279:nerite 251:Attica 216:Rhodes 189:flysch 179:, the 155:Eocene 133:. The 131:gypsum 76:marble 53:gneiss 49:schist 34:Greece 932:Ă…land 851:Spain 776:Malta 746:Italy 403:Chios 294:chert 197:Crete 177:Crete 568:ISBN 451:Iron 332:and 253:and 195:and 171:The 129:and 127:marl 118:and 94:and 66:and 51:and 16:The 214:to 979:: 397:: 367:. 301:. 249:, 245:, 24:. 612:e 605:t 598:v 122:-

Index

tectonic plates
Greece
Paleozoic
fossils
amphibolite
schist
gneiss
granite
intrusions
Oligocene
Miocene
Strymonas River
marble
sedimentary rocks
Rhodope Massif
Serbo-Macedonian Massif
African plate
Paxi Zone
Ionian Sea
limestone
Jurassic
Cretaceous
Miocene
marl
gypsum
Ionian Zone
Triassic
neritic limestones
Toarcian
Ionian Basin

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