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Sequence stratigraphy of Miocene sequences Kw2a and m5.4, New Jersey: onshore to offshore correlations.

机译:新泽西州中新世序列Kw2a和m5.4的层序地层学:陆上到海上的相关性。

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摘要

I evaluated the upper lower Miocene Kw2a sequence in onshore New Jersey coastal plain coreholes and nearshore wells and its relationship to composite sequence m5.4 on the New Jersey continental shelf. I used Ocean Drilling Program Leg 174AX Cape May Zoo (CMZ) and Ocean View (OV) corehole and well log data to construct the anatomy of composite Kw2a sequence by integrating lithologic changes, grain size data, gamma ray logs, and benthic foraminiferal biofacies and paleodepths in a sequence stratigraphic framework. I identified 3 higher order sequences (Kw2a1, Kw2a2, and Kw2a3) and stratal boundaries (transgressive surfaces [TS] and maximum flooding surfaces [MFS]) within the composite Kw2a sequence. A thin, deepening upward LST is tentatively identified only at the base of the Kw2a1 higher order sequence at both sites. Mud dominant, deepening and fining upward TST's are found in all 3 higher order sequences. MFS are associated with mud and Uvigerinaspp. peaks and are overlain by, sandy coarsening and shallowing upward HST's. To test the physical correlation between onshore-nearshore and middle shelf systems, I identified Kw2a and higher order sequences in other ODP Leg 150A, 174AX, and U.S.G.S onshore and nearshore wells using gamma ray logs. I correlated gamma ray logs of the composite Kw2a sequence to onshore [Atlantic City (AC)] and nearshore wells (ACOW-1, 2, AMCOR-6011) and traced the Kw2a sequence on seismic profiles crossing these sites. I projected other onshore cores and logs to nearby seismic profiles. I traced the composite Kw2a sequence on seismic profiles directly to IODP Expedition 313 coreholes where I demonstrate that the composite Kw2a sequence is physically equivalent to composite m5.4 sequence.
机译:我评估了新泽西州沿海沿海平原岩心孔和近岸井中的中新世下部Kw2a序列及其与新泽西大陆架上的m5.4组合序列的关系。我使用海洋钻探计划腿174AX开普梅动物园(CMZ)和海洋景观(OV)井眼和测井数据,通过整合岩性变化,粒度数据,伽马射线测井和底栖有孔虫生物相,构造了复合Kw2a序列的解剖结构层序地层框架中的古深度。我确定了复合Kw2a序列中的3个高阶序列(Kw2a1,Kw2a2和Kw2a3)和层间边界(海侵面[TS]和最大洪泛面[MFS])。暂时仅在两个位点的Kw2a1高阶序列的底部临时确定了一个薄的,加深的向上LST。在所有3个高阶序列中都发现了泥浆占主导地位,向上加深和细化的TST。 MFS与泥浆和Uvigerinaspp相关。高峰,并被HST的砂质粗化和浅化所覆盖。为了测试陆上-近海和中陆架系统之间的物理相关性,我使用伽马射线测井仪确定了其他ODP Leg 150A,174AX和U.S.G.S陆上和近岸井中的Kw2a和更高阶序列。我将复合Kw2a序列的伽马射线测井与陆上[Atlantic City(AC)]和近海井(ACOW-1,2,AMCOR-6011)相关联,并在穿越这些站点的地震剖面上追踪了Kw2a序列。我将其他陆上岩心和测井投影到附近的地震剖面。我在地震剖面上直接将合成Kw2a序列追踪到IODP Expedition 313岩心孔,在这里我证明了合成Kw2a序列在物理上等同于合成m5.4序列。

著录项

  • 作者

    Iscimen, Turan.;

  • 作者单位

    Rutgers The State University of New Jersey - New Brunswick.;

  • 授予单位 Rutgers The State University of New Jersey - New Brunswick.;
  • 学科 Geology.;Marine Geology.;Sedimentary Geology.
  • 学位 M.S.
  • 年度 2014
  • 页码 95 p.
  • 总页数 95
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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