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On a Proposed Separation of the so-called Caradoc Sandstone into two district Groups; viz. (1) May Hill Sandstone; (2) Caradoc Sandstone

机译：拟议将所谓的卡拉多砂岩分离成两个地区群体; viz。（1）五月山砂岩; （2）卡拉多克砂岩

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1. PETROGRAPHY OF SANDSTONES OF THEKOPILIFORMATION, JAINTIA HILLS DISTRICT, MEGHALAYA [J] . P. K. Das Bulletin of Pure & Applied Sciences, Section F. Geology: An International Research Journal of Geological Sciences . 2008,第1a2期

机译：梅加莱亚詹蒂亚·希尔斯分布地区千层形砂岩的岩石照相
2. Occurrence of sandstone-type uranium mineralization in the Umthongkut area, Mahadek Basin, West Khasi Hills District, Meghalaya, India [J] . Kothari P. K., Majumdar Amit, Srivastava S. K., Current science . 2008,第12期

机译：印度梅加拉亚邦西卡西山地区马哈德克盆地Umthongkut地区砂岩型铀矿的成因
3. Provenance of the Late Cretaceous Mahadek Sandstones occuring around Mawsynram, East Khasi Hills District, Meghalaya [J] . P. Barthakur, P. K. Das, Anima Gogoi Bulletin Iga . 2006,第1a2期

机译：梅加拉亚邦东卡西希尔斯地区Mawsynram附近发生的晚白垩世Mahadek砂岩成因
4. PALAEOGEOGRAPHY OF EARLY CRETACEOUS WONIWOGI AND TORO SANDSTONES, AND LATE JURASSIC KOPAI SANDSTONE IN PAPUA REGION (INDONESIA) AND PAPUA NEW GUINEA [C] . RM Iman Argakoesoemah Annual convention of the indonesian petroleum association . 2018

机译：早期白垩纪Woniwogi和Toro Sandstones的古地理和巴布亚地区的晚侏罗索科普砂岩（印度尼西亚）和巴布亚新几内亚
5. Controls on Deposition, Lithologic Variability, and Reservoir Heterogeneity of Prolific Western Interior Shelf Sandstone Reservoirs: Tocito and El Vado Sandstones, San Juan Basin, NM [D] . Cheney, Alexander K. 2018

机译：西部内部陆架多产砂岩储层的沉积，岩性变异性和储层非均质性控制：新墨西哥州圣胡安盆地Tocito和El Vado砂岩
6. Population Genetic Structure of a Sandstone Specialist and a Generalist Heath Species at Two Levels of Sandstone Patchiness across the Strait of Gibraltar [O] . Manuel Jesús Gil-López, José Gabriel Segarra-Moragues, Fernando Ojeda -1

机译：直布罗陀海峡两级砂岩斑块状的砂岩专家和通体荒地物种的种群遗传结构
7. Figure 5: (A) SW view of a meseta on the background, taken from the A19 road; (B) amphitheatre outcrop (Tz 21), preserving Cenozoic reddish deposits over older sequences; (C) outcrop along the Muhuesi river (Tz 36), with cross trough stratified sandstones of the Mahogo Formation; (D) river bank outcrop north of the Muhuesi river (Tz 44) with calcretes in the Mbaragandu Formation; (E) outcrop along the Lukoswe river (Tz 40) with stratified sandstones (Mkuju Formation) over massive mudstones (Mbaragandu Formation); (F) carbonate concretions in the Mbaragandu Formation (Tz 43); (G) outcrop at the Zinzima river (Tz 18), with laminated mudstones, with climbing ripples; (H) outcrop along the Mkundi river (Tz48), with low-angle stratified sandstones of the Mkuju Formation over the massive mudstones of the Luwegu Formation. [O] . -1

机译：图5：（a）在背景中的一个meseta的Sw视图，从A19路上采取; （b）圆形剧场露头（TZ 21），在较老序列中保留新生代红沉积物; （c）沿着Muhuesi River（TZ 36）的露出，带有Cross Trough的摩托摩擦砂岩; （d）河北河畔北京北部（TZ 44），曼加大学的群体; （e）沿着卢克韦河（TZ 40）露出巨大的砂岩（MKUJU形成）在大规模的泥岩上（Mbaragandu形成）; （f）Mbaragandu形成中的碳酸盐凝固（TZ 43）; （g）Zinzima River（TZ 18）的露出，带有层压的泥岩，具有攀爬涟漪; （h）沿着Mkundi河（TZ48）露出，用MKUJU的低角度分层砂岩形成，在陆扣式泥土形成的巨大泥岩上。

On a Proposed Separation of the so-called Caradoc Sandstone into two district Groups; viz. (1) May Hill Sandstone; (2) Caradoc Sandstone

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