عنوان مقاله :
رخساره هاي كربناتي در واحد شيلي سازند لالون : يافته هاي نو در ناحيه تويه - دروار (جنوب باختري دامغان )
عنوان به زبان ديگر :
Carbonate Facies of the Shale Unit of the Lalun Formation:New Findings in Tuyeh -Darvar Area (Southwest of Damghan)
اطلاعات موجودي :
فصلنامه سال 1383 شماره 54
كليدواژه :
زمين شناسي , Top Quartzite unit , Lalun Formation , واحد شيلي , estuary , رخساره هاي كربناتي , Sequence stratigraphy , سازند لالون , Bioherm , ناحيه تويه - دروار , جنوب باختري دامغان , Shale unit
چكيده لاتين :
The shale unit of the Lalun Formation in Tuyeh-Darvar area (Southwest of Damghan) is unconformably underlain by the sandstone unit and is gradationally overlain by Top Quartzite unit of the Lalun Formation. The shale unit of the Lalun Formation is composed of siliciclastic facies and two carbonate horizons (less than two meters thick) in the lower part of the shale unit. These carbonate horizons include dolomitized microbialite and ooide grainstone facies, which were deposited in a estuary environment of the northwestern passive margin of Gondwana, following late Early Cambrian mass extinction.
اطلاعات موجودي :
فصلنامه با شماره پیاپی 54 سال 1383
كلمات كليدي :
#تست#آزمون###امتحان