CRETACEOUS SHALLOW MARINE CLASTIC AND BRACKISH TO FRESH-WATER DEPOSITS IN ALBANIA

被引：2
作者：
PEZA, LH
THEODHORI, P
机构：
[1] Instituti Studimeve dhe Projektimeve tè Gjeologjisè, Tirana
来源：
CRETACEOUS RESEARCH | 1993年 / 14卷 / 02期
关键词：
ALBANIA; CRETACEOUS; SHALLOW MARINE; BRACKISH FRESH-WATER FACIES; ALBANIAN ALPS ZONE; MIRDITA ZONE;
D O I：
10.1006/cres.1993.1013
中图分类号：
P5 [地质学];
学科分类号：
0709 ; 081803 ;
摘要：
Cretaceous siliciclastic facies are distinguished in the Mirdita zone, Albania. The shallow marine facies are represented by alternating sandstones, conglomerates and brackish/freshwater charophytic limestones that contain ostracods alternating with algal limestones. This latter facies is predominant in the Albanian Alps zone (Malesia Madhe subzone), and less so in the Mirdita zone. © 1993 by Academic Press, Inc.
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页码：191 / 197
页数：7
相关论文
共 12 条
  • [1] Peza L., 1966, Permbl Stud Min Minier Geol Tirane, V4, P127
  • [2] PEZA L, 1985, B SHKENCAVE GJEOLLOG, V1, P41
  • [3] Peza L.H., 1989, P483
  • [4] PEZA LH, 1988, ARK I STUDIMEVE DHE
  • [5] PEZA LH, 1983, B SHKENCAVE GJEOLOGJ, V4, P71
  • [6] PEZA LH, 1988, B SHKENCAVE GJEOLOGJ, V1, P95
  • [7] PEZA LH, 1985, ARK I STUDIMEVE DHE
  • [8] PEZA LH, 1981, ARK I STUDIMEVE DHE
  • [9] PEZA LH, 1973, ARK I STUDIMEVE DHE
  • [10] PEZA LH, 1985, B SHKENCAVE GJEOLOGJ, V2, P33
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